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Updated Rupice Mineral Resource Estimate

1 Sep 2020 07:00

RNS Number : 5481X
Adriatic Metals PLC
01 September 2020
 

 

Adriatic Metals PLC 

('Adriatic Metals' or the 'Company')

 

UPDATED RUPICE MINERAL RESOURCE ESTIMATE AND DRILLING RESULTS 

To see the images referred to in the release, please click here 

http://www.rns-pdf.londonstockexchange.com/rns/5481X_1-2020-8-31.pdf

 

HIGHLIGHTS: 

Indicated and Inferred Mineral Resource estimate ("MRE") for Adriatic Metals' 100%-owned Rupice silver-gold-zinc-lead deposit in Bosnia & Herzegovina, now stands at:

12.0Mt @ 149g/t Ag, 1.4g/t Au, 4.1% Zn, 2.6% Pb, 0.5% Cu, 25% BaSO4 (reported above a cut-off grade of 50g/t AgEq) containing 58Moz Ag, 527koz Au, 489kt Zn & 312kt Pb

This represents a 32% increase in tonnes compared to the maiden 2019 Rupice MRE (using a 50g/t AgEq cut-off).

79% of the updated Mineral Resource is classified as Indicated.

The updated MRE will provide the foundation to the PFS, which will incorporate ongoing metallurgical test work results and mining studies designed to optimise and improve the planned development configuration of the project compared with that outlined in the November 2019 Scoping Study.

Recent drilling has also intersected high-grade massive sulphide mineralisation at Rupice - with the system remaining open towards the north and down-dip to the south.

 

Adriatic Metals Plc (ASX:ADT, LSE:ADT1) ("Adriatic" or the "Company") is pleased to announce the updated Mineral Resource estimate for the Rupice Silver Deposit in the Vares Silver Project, in Bosnia & Herzegovina, which has been completed by CSA Global Pty Ltd ("CSA Global").

Paul Cronin, Adriatic's Managing Director and CEO commented, "I am thrilled that we have substantially increased our resource base as we go into the next stage of project development. This updated MRE shows the world class nature of the deposit and positions the Company as one of the leading silver developers in the industry." He also added "During the COVID-19 pandemic, I have been impressed by the resolve of our Vares based team to deliver results in a timely and safe manner. Rupice is an exceptionally high-grade silver dominant deposit, and the increase in tonnes will expand on the results of our 2019 Scoping Study, as we seek to finalise a Pre-Feasibility Study in the coming weeks."

MRE UPDATE 

The updated Indicated and Inferred Mineral Resource estimate was prepared by CSA Global in Perth and comprises 12.0 Mt at 149 g/t Ag, 1.4g/t Au, 4.1% Zn and 2.6% Pb, as set out in Table 1.

 

Table 1 - Rupice updated MRE by Classification

 

Rupice Mineral Resources, August 2020

JORC Classification

Tonnes (mt)

Grades

Contained metal

Ag

Zn

Pb

Au

Cu

Sb

BaSO4

Ag

Zn

Pb

Au

Cu

Sb

BaSO4

g/t

%

%

g/t

%

%

%

Moz

Kt

Kt

Koz

Kt

kt

Kt

Indicated

9.5

176

4.9

3.1

1.6

0.5

0.2

29

54

466

294

500

52

22

2,732

Inferred

2.5

49

0.9

0.7

0.3

0.2

0.1

9

4

23

18

27

4

3

218

Total

12.0

149

4.1

2.6

1.4

0.5

0.2

25

58

488

312

526

56

24

2,949

 

Notes:

· Mineral Resources are based on JORC Code definitions.

· A cut-off grade of 50g/t silver equivalent has been applied.

· AgEq - Silver equivalent was calculated using conversion factors of 31.1 for Zn, 24.88 for Pb, 80.0 for Au, 1.87 for BaSO4, 80.87 for Cu and 80.87 for Sb, and recoveries of 90% for all elements. Metal prices used were US$2,500/t for Zn, US$2,000/t for Pb, $150/t for BaSO4, $2,000/oz for Au, $25/oz for Ag, $6500/t for Sb and $6,500 for Cu.

· The applied formula was: AgEq = Ag(g/t) * 90% + 31.1 * Zn(%) * 90% + 24.88 * Pb(%) * 90% + 1.87 * BaSO4% * 90% + 80 * Au(g/t) * 90% + 80.87 * Sb(%) * 90% + 80.87 * Cu(%)* 90%

· It is the opinion of Adriatic Metals and the Competent Persons that all elements and products included in the metal equivalent formula have a reasonable potential to be recovered and sold.

· Metallurgical recoveries of 90% have been applied in the metal equivalent formula based on recent and ongoing test work results.

· A bulk density was calculated for each model cell using regression formula BD = 2.745 + BaSO4 * 0.01793 + Pb * 0.06728 - Zn * 0.01317 + Cu * 0.1105 for the halo domain, BD = 2.7341 + BaSO4 * 0.01823 + Pb * 0.04801 + Zn * 0.03941 - Cu * 0.01051 for the fault zones and BD = 2.7949 + BaSO4 * 0.01599 + Pb * 0.05419 + Zn * 0.01169 + Cu * 0.06303 for the low grade domain. Bulk density values were interpolated to the combined high-grade domain from 631 BD measurements.

· Rows and columns may not add up exactly due to rounding.

 

RUPICE DRILLING AND SAMPLING 

For the Mineral Resource estimate, a total of 167 diamond drill holes (46 historical drill holes and 121 drill holes from the Company's drilling programmes in 2017 (8 holes), 2018 (39 holes), 2019 (52 holes) and 2020 (22 holes)) for 38,135m define the current limits of the known mineralisation. The deposit was drilled and sampled using diamond drill holes at a nominal 20m by 20m spacing.

 

Drill holes drilled by the Company were generally angled -50° to -80° mostly towards the southwest with dip angles set to optimally intersect the mineralised bodies. Additional drill holes were drilled from the opposite direction, and perpendicular to the mineralised trend. All the historical holes were vertical and focussed on the up-dip portion of the Rupice mineralisation.

 

The drill core was sampled for assay; whole core for the historical drilling and half core (HQ and PQ) for the recent drilling. Recent assays were sent to ALS in Bor, Serbia for multi-element analyses.

RUPICE GEOLOGY AND MINERALISATION

 

The host rocks at Rupice comprises Middle Triassic limestone, dolostone, calcareous and dolomitic marl, and a range of mostly fine-grained siliciclastic rocks including cherty mudstone, mudstone, siltstone and fine-grained sandstone. The main mineralised horizon is a brecciated dolomitic unit that dips at around 50o to the northeast and has been preferentially mineralised with base, precious and transitional metals. The Triassic sequence has been intensely deformed both by early stage ductile shearing and late stage brittle faulting.

The Rupice polymetallic mineralisation consists of sphalerite, galena, barite and chalcopyrite with silver, gold, tetrahedrite, boulangerite and bournonite, with pyrite. The majority of the high-grade mineralisation is hosted within the brecciated dolomitic unit, which is offset and cut by northwest striking, westerly dipping syn-post mineral faulting. This faulting displaces the mineralised body up to 20 metres in places. Thickening of the central portion of the orebody occurs where these faults flexure and deform. Mineralised widths up to 65 metres true thickness are seen in the central portion of the orebody.

To date, the massive sulphide mineralisation at Rupice has a defined strike length of 650 metres, with an average true-width thickness of around 20 metres. However, mineralisation at Rupice still remains open towards the north and down-dip to the south.

RUPICE MODELLING AND GRADE INTERPOLATION

The main geological features that control the polymetallic mineralisation at Rupice were interpreted using geological and structural data collected. Three main domains were interpreted and wireframed individually; the main mineralised brecciated dolomitic units, that hosts the high-grade mineralisation; the fault zones that off-set and displace these main mineralised bodies; and a lower-grade halos peripheral and in the footwall of the main mineralised bodies.

Statistical analysis of modelled domains showed that the main mineralised brecciated dolomite has a bimodal population for the majority of the elements being modelled. The higher-grade populations clustered spatially and were subsequently individually interpreted and wireframed.

Ten elements were modelled; Ag, Zn, Pb, BaSO4, Cu, Au, Sb, Hg, As and S, and the higher-grade populations were interpreted and wireframed for all elements except Hg, As and Sb.

All the domains were interpreted on a section by section basis and were used to generate 3D 'solid' wireframes. The same methodology was applied for the individual high-grade populations.

Once mineralisation for each element was interpreted and wireframed, classical statistical analysis was repeated for the samples within the interpreted domains. Drill data was composited to 2m down hole intervals. Boundary statistical analyses and top cuts were determined and applied.

The geostatistical analysis generated a series of semi-variograms that were used during grade estimation using Ordinary Kriging ("OK"). The semi-variogram ranges determined from the analysis contribute heavily to the determination of the search neighbourhood dimensions. All variograms were calculated and modelled for the composited sample file, constrained by the corresponding mineralised envelopes for each element. Where low-grade and high-grade domains were modelled, samples were combined for both domains to make sure that the number of samples was sufficient for robust geostatistical analysis. It was found that absolute semi-variograms were difficult to model for most of elements, and therefore, relative semi-variograms were modelled for Pb, BaSO4, Ag, Au, Sb, Hg, As and Cu. Absolute variograms were modelled for Zn and S.

The density values were calculated for each model cell using a regression formula for all the domains except the combined high-grade domain. The formula was calculated using scattergrams for density versus BaSO4, Pb, Cu and Zn grades. Density values were interpolated within the limits of the combined high-grade domain.

A block model was constructed, constrained by the interpreted mineralised envelopes. A parent cell size of 5 m(E) x 5 m(N) x 5 m(RL) was adopted with standard sub-celling to 1 m(E) x 1 m(N) x 1 m(RL) to maintain the volumetric resolution of the mineralised lenses.

Grades for all ten elements were interpolated into the empty block model using the Ordinary Kriging method and a "parent block estimation" technique, i.e. all sub-cells within a parent cell were populated with the same grade. The OK process was performed at different search radii until all cells were interpolated. The search radii were determined by means of the evaluation of the semi-variogram parameters, which determined the kriging weights to be applied to samples at specified distances.

Block grades were validated both visually and statistically and all modelling was completed using Micromine software.

RUPICE CLASSIFICATION AND REPORTING

Clause 20 of the JORC (2012) Code requires that all reports of Mineral Resources must have reasonable prospects for eventual economic extraction, regardless of the classification of the resource. The Rupice deposit has reasonable prospects for eventual economic extraction on the following basis:

 

· Metallurgical test work by WAI has confirmed that the Rupice mineralisation is amenable to flotation processes;

· Preliminary metallurgical test work has confirmed that a barite concentrate should meet API specifications;

· A marketing study by a leading consultant in the field of barite confirmed that there is an opportunity to enter the market as a niche player levering any logistical advantages for a supplier in Bosnia & Herzegovina;

· The cut-off grade adopted for reporting (50g/t Ag equivalent) is considered reasonable given the Mineral Resource will most likely be exploited by underground mining methods and processed using flotation techniques.

The Scoping Study demonstrated that the deposit potentially has a positive net present value (NPV), and that the mineralised zone is potentially mineable using underground methods under the given economic scenario and parameters. CSA Global did not estimate Ore Reserves for the deposit. The deposit appears to have reasonable prospects of eventual economic extraction under a realistic set of criteria.

The Rupice Mineral Resource has been classified based on the guidelines specified in the JORC Code. The classification level is based upon an assessment of geological understanding of the deposit, geological and mineralisation continuity, drill hole spacing, QC results, search and interpolation parameters and an analysis of available density information. The MRE is reported by classification in Table 1, above a cut-off grade of 50g/t silver equivalent.

RECENT DRILL RESULTS

The Company is pleased to announce that it has received assay results from BR-10-20, BR-11-20, BR-12-20, BR-13-20, BR-17-20, BR-18-20, BR-20-20, BR-22-20 and BR-23-20, which have been incorporated into the recent Mineral Resource estimate.

Drillhole BR-20-20 (Figure 7) is the most southern drill hole drilled at Rupice to date. It was designed to test the extension of the Rupice orebody along strike to the southeast. The results from this hole have shown that the massive sulphide mineralisation continues southwards. Follow up drilling will test the continuity of mineralisation to the south, up-dip and down-dip from this intercept.

Drillholes BR-11-20, BR-12-20 (Figure 5) and BR-13-20 (Figure 5) successfully intersected mineralisation. They were designed to test the shallower part of the deposit to the south-west, and to confirm historic drilling results.

BR-17-20 and BR-18-20 (Figure 6) were designed to test the up-dip continuation of the known massive sulphide mineralisation in the central part of the deposit. They were also designed to test potential massive sulphide mineralisation in the footwall of the main mineralised body. Higher grade mineralisation was intercepted in two shorter intervals up-dip from the main mineralised body in BR-17-20, followed by a wider low-grade halo in the footwall of the deposit.

For BR-18-20, massive sulphide mineralisation was encountered up-dip from the main mineralised body, confirming continuity of the known mineralised zone.

Drill hole BR-14-20 in the northern part Rupice, and BR-15-20 in the south-western part of Rupice were also drilled. These were designed as investigate continuity of mineralised zone. Mineralisation was encountered, however of a weaker tenor.

Mineralisation still remains open down-dip and to the south and north, into previously untested ground outside of the current ore block model.

The mineralised intervals of the drill holes are shown in Table 2 with further information in Appendix 1. 

Table 2 - Drill Hole Results for the Reported Holes; Lead or Zinc greater than 1%,

Hole

From (m)

To

(m)

Interval (m)

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4 %

BR-10-20

204.0

206.0

2.0

2.45

1.24

0.45

16

0.07

0

BR-11-20

62.2

67.0

4.8

1.68

1.73

0.66

150

0.51

56

BR-12-20

113.5

116.4

2.9

4.52

3.44

1.29

224

0.29

32

BR-13-20

123.5

134.9

11.4

2.39

1.58

0.69

54

0.55

14

BR-17-20

204.0

206.0

2.0

1.85

0.82

0.89

141

0.27

26

BR-18-20

174.7

183.7

9.0

1.85

1.39

0.99

152

0.82

51

BR-20-20

228.2

238

9.8

1.62

1.50

0.55

106

0.45

24

BR-22-20

307.0

311.0

4.0

1.28

0.32

0.04

28

0.01

4

BR-23-20

329.0

338.6

9.6

5.01

5.03

1.28

431

0.60

57

 

Drilling at Jurasevac-Brestic was also conducted, designed to test the gravity anomaly defined after data reprocessing in March this year. Five diamond drill holes targeted the main gravity high, and massive and patchy pyrite, and weak lead, zinc and barite mineralisation was encountered. Drilling proved the validity of the gravity anomaly, however, economic mineralisation has not been encountered so far.

Exploration and hydrological drilling works continue on the Vares Silver Project with two rigs testing the mineralisation further southward at Rupice, and one at Veovaca drilling geotechnical and hydrological holes. More drillholes are planned for testing the extensions of Rupice deposit to the south and down-dip.

Authorised by, and for further information please contact: Paul CroninManaging Director & CEOinfo@adriaticmetals.com

 

** ENDS **

Market Abuse Regulation Disclosure

The information contained within this announcement is deemed by Adriatic (LEI: 549300OHAH2GL1DP0L61) to constitute inside ‎information as stipulated under the Market Abuse Regulations (EU) No. 596/2014. The person ‎responsible for arranging and authorising the release of this announcement on behalf of Adriatic is Paul Cronin, Managing Director and CEO.

For further information please visit www.adriaticmetals.com; @AdriaticMetals on Twitter; or contact:

Adriatic Metals PLC

 

Paul Cronin / Emma Chetwynd Stapylton

Tel: +44 (0) 203 950 9138

 

 

Tavistock Communications Limited

 

Charles Vivian

Tel: +44 (0) 7977 297903

Edward Lee

Tel: +44 (0) 7736 220565

Gareth Tredway

Tel: +44 (0) 7785 974264

 

 

The Capital Network

 

Julia Maguire/Lelde Smits

Tel: +61 2 8999 3699

 

About Adriatic Metals

Adriatic Metals Plc (ASX:ADT, LON:ADT1) is a precious and base metals explorer and developer that owns the world-class advanced polymetallic Vares project in Bosnia & Herzegovina.

The Vares project consists of two high-grade polymetallic deposits, located at Rupice and Veovaca. Bosnia & Herzegovina is well-positioned in central Europe and boasts a strong mining history, pro-mining environment, highly-skilled workforce as well as extensive existing infrastructure and logistics.

The Vares project's captivating economics and impressive resource inventory have attracted Adriatic's highly experienced team, which is expediting exploration efforts to expand the current JORC resource. Results of a recent scoping study indicate an NPV8 of US$917 million and IRR of 107%. Leveraging its first-mover advantage, Adriatic is rapidly advancing the project into the development phase and through to production.

There have been no material adverse changes in the assumptions underpinning the forecast financial information or material assumptions and technical parameters underpinning the Maiden Resource Estimate since the original relevant market announcements which continue to apply.

COMPETENT PERSONS REPORT

The information in this report that relates to the Mineral Resources is based on and fairly represents information and supporting information compiled by Dmitry Pertel. Dmitry Pertel is a full-time employee of CSA Global and is a Member of the Australian Institute of Geoscientists. Dmitry Pertel has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for the Reporting of Exploration Results, Mineral Resources, and Ore Reserves (JORC Code). Dmitry Pertel consents to the disclosure of information in this report in the form and context in which it appears.

 

The information in this report which relates to Exploration Results is based on and fairly represents information and supporting information compiled by Mr Phillip Fox, who is a member of the Australian Institute of Geoscientists (AIG). Mr Fox is a consultant to Adriatic Metals Plc, and has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the "Australian Code of Reporting of Exploration Results, Mineral Resources and Ore Reserves". Mr Fox consents to the inclusion in this report of the matters based on that information in the form and context in which it appears.

DISCLAIMER

Forward-looking statements are statements that are not historical facts. Words such as "expect(s)", "feel(s)", "believe(s)", "will", "may", "anticipate(s)", "potential(s)"and similar expressions are intended to identify forward-looking statements. These statements include, but are not limited to statements regarding future production, resources or reserves and exploration results. All of such statements are subject to certain risks and uncertainties, many of which are difficult to predict and generally beyond the control of the Company, that could cause actual results to differ materially from those expressed in, or implied or projected by, the forward-looking information and statements. These risks and uncertainties include, but are not limited to: (i) those relating to the interpretation of drill results, the geology, grade and continuity of mineral deposits and conclusions of economic evaluations, (ii) risks relating to possible variations in reserves, grade, planned mining dilution and ore loss, or recovery rates and changes in project parameters as plans continue to be refined, (iii) the potential for delays in exploration or development activities or the completion of feasibility studies, (iv) risks related to commodity price and foreign exchange rate fluctuations, (v) risks related to failure to obtain adequate financing on a timely basis and on acceptable terms or delays in obtaining governmental approvals or in the completion of development or construction activities, and (vi) other risks and uncertainties related to the Company's prospects, properties and business strategy. Our audience is cautioned not to place undue reliance on these forward-looking statements that speak only as of the date hereof, and we do not undertake any obligation to revise and disseminate forward-looking statements to reflect events or circumstances after the date hereof, or to reflect the occurrence of or non-occurrence of any events.

 

Table 3 - Collar Information for reported drill holes (MGI Balkans Z6)

Drill Hole

Easting

Northing

Elevation

Average Azimuth (TN)

Average Dip

Depth (m)

BR-10-20

6519271

4894736

1206

58

-85

373.6

BR-11-20

6519241

4894518

1212

226

-61

184.0

BR-12-20

6519275

4894592

1217

227

-55

130.1

BR-13-20

6519275

4894592

1217

228

-71

155.2

BR-17-20

6519079

4894785

1162

54

-73

498.5

BR-18-20

6519151

4894717

1187

64

-85

607.0

BR-20-20

6519446

4894547

1265

231

-73

252.2

BR-22-20

6519216

4894898

1124

149

-86

312.7

BR-23-20

6519411

4894627

1264

223

-90

368.0

 

 

 

 

 

Table 4 - Assay Results for reported drill holes

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-10-20

0

1

1

0.0054

0.0011

0.0025

0.0044

0.015

BR-10-20

1

2.5

1.5

0.0071

0.001

0.0044

0.015

BR-10-20

2.5

4.5

2

0.0166

0.0053

0.0034

0.015

BR-10-20

4.5

6.5

2

0.008

0.0026

0.0027

0.015

BR-10-20

6.5

7.5

1

0.0055

0.0012

0.008

0.0038

0.015

BR-10-20

7.5

9.5

2

0.01

0.001

0.0045

0.015

BR-10-20

9.5

11.5

2

0.0164

0.0015

0.0042

0.015

BR-10-20

11.5

13.5

2

0.019

0.0059

0.0038

0.015

BR-10-20

13.5

14.4

0.9

0.0257

0.0092

0.0037

0.015

BR-10-20

14.4

16.4

2

0.0075

0.0062

0.0015

0.015

BR-10-20

16.4

17.6

1.2

0.0079

0.0068

0.0022

0.015

BR-10-20

17.6

19

1.4

0.0139

0.0167

0.005

0.006

0.03

BR-10-20

19

21

2

0.0174

0.0327

0.011

0.0048

0.015

BR-10-20

21

23

2

0.0112

0.0217

0.003

0.015

BR-10-20

23

25

2

0.006

0.0045

0.006

0.0035

0.03

BR-10-20

25

27

2

0.0103

0.0195

0.0037

0.03

BR-10-20

27

28.2

1.2

0.0101

0.0224

0.007

0.0041

0.03

BR-10-20

28.2

30

1.8

0.0088

0.0122

0.005

0.0036

0.015

BR-10-20

30

32

2

0.0083

0.0101

0.007

0.004

0.03

BR-10-20

32

34

2

0.0081

0.0107

0.01

0.0037

0.015

BR-10-20

34

36

2

0.0075

0.0176

0.005

0.0038

0.015

BR-10-20

36

38

2

0.0086

0.0212

0.0042

0.015

BR-10-20

38

40

2

0.01

0.0091

0.006

0.0057

0.015

BR-10-20

40

42

2

0.027

0.0222

0.005

0.0041

0.015

BR-10-20

42

43.3

1.3

0.0292

0.0276

0.0032

0.015

BR-10-20

43.3

44.9

1.6

0.0132

0.0426

0.0067

0.03

BR-10-20

44.9

46

1.1

0.0138

0.0169

0.0021

0.015

BR-10-20

46

48

2

0.0234

0.0155

0.006

0.0039

0.015

BR-10-20

48

50

2

0.0227

0.0231

0.003

0.03

BR-10-20

50

51.9

1.9

0.0124

0.0121

0.0013

0.046

BR-10-20

51.9

53

1.1

0.0094

0.0098

0.0011

0.015

BR-10-20

53

55

2

0.0109

0.0371

0.0033

0.03

BR-10-20

55

57

2

0.0066

0.0042

0.0017

0.03

BR-10-20

57

59

2

0.0231

0.0244

0.0128

0.046

BR-10-20

59

60.3

1.3

0.0528

0.0179

0.005

0.0033

0.046

BR-10-20

60.3

63.2

2.9

No sample

BR-10-20

63.2

65

1.8

0.0067

0.0132

0.012

0.106

BR-10-20

65

67

2

0.0095

0.0232

0.011

0.0063

0.213

BR-10-20

67

69

2

0.0067

0.0175

0.008

0.0031

0.061

BR-10-20

69

71

2

0.0063

0.0061

0.009

0.0041

0.046

BR-10-20

71

73

2

0.0055

0.0036

0.0026

0.046

BR-10-20

73

74.4

1.4

0.0101

0.0115

0.0037

0.046

BR-10-20

74.4

74.9

0.5

No sample

BR-10-20

74.9

76.6

1.7

0.0074

0.0059

0.005

0.0042

0.03

BR-10-20

76.6

78

1.4

0.0175

0.0069

0.007

0.0117

0.046

BR-10-20

78

80

2

0.0119

0.0055

0.0059

0.03

BR-10-20

80

82

2

0.0153

0.0076

0.0057

0.03

BR-10-20

82

84

2

0.0266

0.0434

0.006

0.0096

0.03

BR-10-20

84

85

1

0.0182

0.0282

0.0083

0.046

BR-10-20

85

86.5

1.5

0.0179

0.0136

0.006

0.5

0.0091

0.03

BR-10-20

86.5

88

1.5

0.0195

0.0029

0.006

0.0073

0.03

BR-10-20

88

90

2

0.0114

0.0063

0.011

0.0078

0.03

BR-10-20

90

91.4

1.4

0.0119

0.0079

0.008

0.0082

0.015

BR-10-20

91.4

93

1.6

0.0139

0.0048

0.008

0.0068

0.03

BR-10-20

93

95

2

0.0117

0.0035

0.0046

0.03

BR-10-20

95

95.9

0.9

0.0109

0.0026

0.0041

0.015

BR-10-20

95.9

97

1.1

0.0082

0.0021

0.0027

0.015

BR-10-20

97

99

2

0.0087

0.002

0.0024

0.015

BR-10-20

99

100.7

1.7

0.0094

0.003

0.007

0.015

BR-10-20

100.7

102

1.3

0.0072

0.0065

0.0021

0.015

BR-10-20

102

104

2

0.0097

0.0071

0.0013

0.015

BR-10-20

104

106

2

0.0097

0.007

0.0014

0.015

BR-10-20

106

108

2

0.0113

0.0087

0.002

0.015

BR-10-20

108

110

2

0.0141

0.0095

0.0023

0.015

BR-10-20

110

111

1

0.0247

0.0121

0.0039

0.03

BR-10-20

111

112.2

1.2

0.0234

0.0271

0.0048

0.046

BR-10-20

112.2

117.8

5.6

No sample

BR-10-20

117.8

119

1.2

0.0778

0.0479

0.007

1

0.0286

0.046

BR-10-20

119

121

2

0.0368

0.0942

0.6

0.009

0.228

BR-10-20

121

123

2

0.0144

0.0353

0.0014

0.015

BR-10-20

123

125

2

0.0119

0.038

0.0009

0.015

BR-10-20

125

127

2

0.006

0.0524

0.001

0.076

BR-10-20

127

129

2

0.0226

0.172

0.005

1.1

0.0155

0.015

BR-10-20

129

131

2

0.0303

0.2

1.3

0.0091

0.03

BR-10-20

131

132.8

1.8

0.0318

0.15

1.2

0.0037

0.03

BR-10-20

132.8

134

1.2

0.0164

0.0563

0.004

0.046

BR-10-20

134

136

2

0.0229

0.0501

0.061

BR-10-20

136

138

2

0.012

0.0428

0.6

0.0024

0.061

BR-10-20

138

138.5

0.5

0.0123

0.0942

0.0024

0.03

BR-10-20

138.5

139

0.5

No sample

BR-10-20

139

141

2

0.0148

0.028

0.0008

0.015

BR-10-20

141

143

2

0.0178

0.0226

0.0009

0.015

BR-10-20

143

145

2

0.0134

0.0331

0.0015

0.046

BR-10-20

145

147

2

0.0103

0.0088

0.0007

0.137

BR-10-20

147

149

2

0.0195

0.005

0.0021

0.137

BR-10-20

149

151

2

0.0191

0.0047

0.0021

0.091

BR-10-20

151

153

2

0.0122

0.0032

0.0016

0.548

BR-10-20

153

153.8

0.8

0.018

0.0066

0.046

BR-10-20

153.8

155

1.2

0.0105

0.0035

0.0018

0.03

BR-10-20

155

157

2

0.0287

0.008

0.0021

0.03

BR-10-20

157

159

2

0.0127

0.0043

0.0019

0.061

BR-10-20

159

161

2

0.0157

0.004

0.0024

0.137

BR-10-20

161

162.2

1.2

0.0079

0.001

0.009

0.0013

0.213

BR-10-20

162.2

164

1.8

0.0085

0.0003

0.0003

0.106

BR-10-20

164

165.6

1.6

0.0094

0.0011

0.04

0.0033

0.106

BR-10-20

165.6

167

1.4

0.0093

0.0044

0.014

1.8

0.0109

0.669

BR-10-20

167

169

2

0.017

0.005

0.0015

0.715

BR-10-20

169

171

2

0.0267

0.0026

0.0013

0.73

BR-10-20

171

173

2

0.043

0.0651

1.7

0.0055

0.167

BR-10-20

173

175

2

0.0526

0.123

0.005

1.9

0.0067

0.548

BR-10-20

175

175.9

0.9

0.0059

0.013

0.001

0.335

BR-10-20

175.9

177

1.1

0.0114

0.0012

0.0007

0.167

BR-10-20

177

178.4

1.4

0.0131

0.0022

0.01

0.002

0.472

BR-10-20

178.4

180

1.6

0.0429

0.0078

0.014

0.6

0.0027

0.183

BR-10-20

180

182

2

0.0167

0.0082

0.026

1.1

0.0019

0.228

BR-10-20

182

184

2

0.0311

0.0102

0.029

2.3

0.0017

0.38

BR-10-20

184

186

2

0.0796

0.0727

0.047

5.2

0.0064

0.304

BR-10-20

186

188

2

0.0557

0.0348

0.033

23.3

0.0083

0.487

BR-10-20

188

189.9

1.9

0.241

0.0682

0.034

15.7

0.0068

0.593

BR-10-20

189.9

191

1.1

0.0832

0.0343

0.012

3.6

0.0119

0.487

BR-10-20

191

192

1

0.0088

0.004

0.032

0.7

0.0016

0.152

BR-10-20

192

193

1

0.0116

0.0045

0.027

0.5

0.0015

1.034

BR-10-20

193

194

1

0.01

0.0054

0.013

0.6

0.0032

0.441

BR-10-20

194

195

1

0.0106

0.016

0.013

0.7

0.004

0.487

BR-10-20

195

196

1

0.0086

0.0413

0.5

0.0034

1.156

BR-10-20

196

197

1

0.0147

0.0103

2.3

0.0036

0.228

BR-10-20

197

198

1

0.0082

0.0018

0.007

1

0.001

0.046

BR-10-20

198

199

1

0.217

0.127

0.028

6.5

0.0088

8.276

BR-10-20

199

200

1

0.0192

0.017

0.02

6.6

0.0263

1.491

BR-10-20

200

201

1

0.0091

0.0064

1.4

0.0009

1.004

BR-10-20

201

202

1

0.0427

0.0281

0.021

3

0.0045

0.517

BR-10-20

202

203

1

0.0331

0.493

0.165

13.2

0.13

0.578

BR-10-20

203

204

1

0.022

0.0195

0.172

1.1

0.002

0.213

BR-10-20

204

205

1

1.295

0.615

0.354

7.3

0.0351

0.456

BR-10-20

205

206

1

3.6

1.86

0.545

24.8

0.101

0.198

BR-10-20

206

206.9

0.9

0.0594

0.034

0.027

1.5

0.0022

0.806

BR-10-20

206.9

208

1.1

0.0139

0.0235

0.095

0.5

0.0028

1.78

BR-10-20

208

209

1

0.0261

0.0139

0.06

0.0021

0.061

BR-10-20

209

210

1

0.0265

0.0088

0.032

0.0104

0.152

BR-10-20

210

211

1

0.0109

0.0105

0.037

0.002

0.046

BR-10-20

211

212

1

0.024

0.0069

0.027

0.0012

0.046

BR-10-20

212

213

1

0.0113

0.0275

0.023

0.0028

0.046

BR-10-20

213

214

1

0.038

0.222

0.031

1.5

0.0099

0.03

BR-10-20

214

215

1

0.0403

0.288

0.049

2

0.0071

0.061

BR-10-20

215

216

1

0.0451

0.0182

0.055

0.002

0.183

BR-10-20

216

217

1

0.0619

0.0137

0.026

0.0013

0.091

BR-10-20

217

218

1

0.0847

0.014

0.034

0.0016

0.076

BR-10-20

218

219

1

0.0963

0.015

0.187

0.8

0.0033

0.046

BR-10-20

219

220

1

0.173

0.007

0.189

1.2

0.0068

0.015

BR-10-20

220

221

1

0.0986

0.007

0.183

1.4

0.005

0.03

BR-10-20

221

222

1

0.13

0.0075

0.194

1.3

0.0048

0.015

BR-10-20

222

223

1

0.124

0.0062

0.152

0.7

0.0029

0.015

BR-10-20

223

224

1

0.682

0.0389

0.688

10.9

0.119

0.015

BR-10-20

224

225

1

0.0527

0.0086

0.167

1.8

0.0169

0.015

BR-10-20

225

226

1

0.161

0.0126

0.272

2.8

0.0113

0.03

BR-10-20

226

227

1

0.813

0.057

0.764

12.4

0.348

0.122

BR-10-20

227

228

1

0.435

0.0548

0.216

3.2

0.0336

0.35

BR-10-20

228

229

1

0.514

0.081

0.235

3.7

0.0413

0.03

BR-10-20

229

230

1

0.0689

0.0583

0.11

1.5

0.0118

0.472

BR-10-20

230

231

1

0.0708

0.0048

0.042

0.0015

0.578

BR-10-20

231

232

1

0.0466

0.0047

0.056

0.5

0.0036

0.106

BR-10-20

232

233

1

0.0435

0.063

0.0015

0.03

BR-10-20

233

234

1

0.0359

0.0345

0.069

0.5

0.0043

0.015

BR-10-20

234

235

1

0.0402

0.0097

0.056

0.7

0.0017

1.171

BR-10-20

235

236

1

0.0195

0.028

0.116

0.6

0.0027

0.061

BR-10-20

236

237

1

0.0113

0.0069

0.086

0.0016

0.015

BR-10-20

237

238

1

0.0181

0.0049

0.095

0.0015

0.015

BR-10-20

238

239

1

0.0534

0.0051

0.039

0.001

0.03

BR-10-20

239

240

1

0.0118

0.0093

0.051

0.0103

0.03

BR-10-20

240

241

1

0.0279

0.0108

0.055

0.5

0.0022

0.243

BR-10-20

241

242

1

0.0198

0.0259

0.009

0.0004

0.03

BR-10-20

242

243

1

0.0037

0.0106

0.026

0.0002

0.061

BR-10-20

243

244

1

0.154

0.0414

0.026

0.0411

2.601

BR-10-20

244

244.8

0.8

0.0384

0.0066

0.012

0.0007

0.289

BR-10-20

244.8

246

1.2

0.0234

0.006

0.016

0.0017

0.03

BR-10-20

246

247.3

1.3

0.022

0.0005

0.0004

0.015

BR-10-20

247.3

249

1.7

0.013

0.0006

0.0008

0.008

BR-10-20

249

251

2

0.0161

0.0008

0.0002

0.015

BR-10-20

251

253

2

0.0113

0.0005

0.012

0.0001

0.008

BR-10-20

253

255

2

0.0165

0.0008

0.007

0.0002

0.061

BR-10-20

255

257

2

0.017

0.0005

0.007

0.0001

0.008

BR-10-20

257

258.3

1.3

0.0226

0.0004

0.0001

0.008

BR-10-20

258.3

260

1.7

0.0179

0.0011

0.001

0.008

BR-10-20

260

262

2

0.0272

0.002

0.0511

0.046

BR-10-20

262

262.5

0.5

0.0189

0.0007

0.0002

0.03

BR-10-20

262.5

264

1.5

0.0165

0.0006

0.0002

0.03

BR-10-20

264

266

2

0.0491

0.001

0.0006

0.061

BR-10-20

266

266.9

0.9

0.0096

0.001

0.0008

0.046

BR-10-20

266.9

268

1.1

0.0156

0.0008

0.0011

0.03

BR-10-20

268

270

2

0.0138

0.0007

0.005

0.0023

0.046

BR-10-20

270

272

2

0.0223

0.001

0.0007

0.015

BR-10-20

272

273.4

1.4

0.0146

0.0008

0.0003

0.015

BR-10-20

273.4

275

1.6

0.0113

0.0007

0.0005

0.046

BR-10-20

275

277

2

0.0106

0.0012

0.0002

0.046

BR-10-20

277

279

2

0.0093

0.0008

0.0002

0.046

BR-10-20

279

281

2

0.0109

0.0004

0.0001

0.03

BR-10-20

281

283

2

0.0111

0.0004

0.0001

0.046

BR-10-20

283

283.8

0.8

0.0106

0.0008

0.0001

0.046

BR-10-20

283.8

285

1.2

0.0123

0.0005

0.0001

0.03

BR-10-20

285

287

2

0.0082

0.0007

0.0001

0.122

BR-10-20

287

289

2

0.0073

0.001

0.0017

0.38

BR-10-20

289

291

2

0.0241

0.0017

0.007

0.0003

0.122

BR-10-20

291

293

2

0.0192

0.0098

0.048

1.6

0.0045

0.274

BR-10-20

293

294

1

0.014

0.0107

0.037

1.3

0.0023

0.289

BR-10-20

294

295

1

0.0133

0.0056

0.013

0.7

0.0046

0.152

BR-10-20

295

296

1

0.104

0.0503

0.068

3.1

0.0036

0.259

BR-10-20

296

297

1

0.0526

0.0683

0.033

4.5

0.0078

0.243

BR-10-20

297

298

1

0.262

0.18

0.112

7.9

0.0121

0.046

BR-10-20

298

299

1

0.331

0.124

0.174

8.6

0.0139

0.183

BR-10-20

299

300

1

0.191

0.0993

0.066

3.7

0.0054

0.137

BR-10-20

300

301

1

0.0702

0.0156

0.071

2.8

0.0032

0.076

BR-10-20

301

302

1

0.373

0.079

0.122

3.2

0.0051

0.152

BR-10-20

302

303

1

0.0253

0.0047

0.024

1.3

0.0008

0.061

BR-10-20

303

304

1

0.159

0.251

0.085

4.5

0.0063

0.578

BR-10-20

304

305

1

0.235

0.135

0.049

3.5

0.0072

0.365

BR-10-20

305

306

1

0.254

0.345

0.106

6.4

0.0228

0.517

BR-10-20

306

307.2

1.2

0.0908

0.0632

0.078

2.9

0.0091

0.517

BR-10-20

307.2

308.4

1.2

0.135

0.0273

0.021

1.4

0.0009

0.198

BR-10-20

308.4

309.4

1

0.0472

0.0573

0.044

2.4

0.0015

0.882

BR-10-20

309.4

310.6

1.2

0.308

0.114

0.051

4

0.003

0.38

BR-10-20

310.6

311.7

1.1

0.132

0.0393

0.042

4.3

0.0049

0.289

BR-10-20

311.7

312.8

1.1

0.264

0.133

0.08

14

0.0191

0.943

BR-10-20

312.8

314

1.2

0.363

0.324

0.133

23

0.0344

1.978

BR-10-20

314

315

1

0.183

0.0626

0.08

5

0.0065

0.608

BR-10-20

315

316.2

1.2

0.127

0.0218

0.031

1.4

0.0019

0.106

BR-10-20

316.2

317.4

1.2

0.416

0.181

0.119

7.8

0.0217

0.35

BR-10-20

317.4

318.6

1.2

0.29

0.178

0.142

28.4

0.0907

0.152

BR-10-20

318.6

319.8

1.2

0.145

0.0964

0.138

12.7

0.0604

0.091

BR-10-20

319.8

321

1.2

0.599

0.608

0.195

14.4

0.0714

0.548

BR-10-20

321

322

1

0.742

0.432

0.319

18.1

0.0746

0.335

BR-10-20

322

323.2

1.2

0.478

0.224

0.161

6.3

0.015

0.593

BR-10-20

323.2

324

0.8

0.0914

0.0216

0.036

1.2

0.005

0.228

BR-10-20

324

325

1

0.0524

0.0238

0.063

1.1

0.0095

0.396

BR-10-20

325

326

1

0.101

0.0769

0.04

1.3

0.0045

0.685

BR-10-20

326

327

1

0.149

0.0196

0.058

0.7

0.0019

0.137

BR-10-20

327

328

1

0.127

0.0802

0.165

3.9

0.0501

0.608

BR-10-20

328

329

1

0.0658

0.0779

0.104

1.9

0.0155

0.274

BR-10-20

329

330

1

0.0294

0.0806

0.158

1.3

0.0086

0.076

BR-10-20

330

331

1

0.0714

0.0215

0.088

1

0.0051

0.091

BR-10-20

331

332

1

0.0487

0.071

0.075

1.6

0.0143

0.198

BR-10-20

332

333

1

0.0316

0.0447

0.058

1

0.0047

0.122

BR-10-20

333

334

1

0.211

0.317

0.322

6.9

0.108

1.4

BR-10-20

334

335

1

0.142

0.452

0.178

6.5

0.0792

0.487

BR-10-20

335

336

1

0.281

0.653

0.121

9

0.13

0.974

BR-10-20

336

337

1

0.0504

0.0131

0.051

0.0014

0.152

BR-10-20

337

338

1

0.148

0.0659

0.081

1.4

0.0121

0.076

BR-10-20

338

339

1

0.249

0.453

1.655

7.9

0.112

0.091

BR-10-20

339

340

1

0.223

0.311

0.164

13.1

0.296

1.993

BR-10-20

340

341

1

0.264

0.213

0.29

3.8

0.0657

0.532

BR-10-20

341

342

1

0.028

0.0188

0.093

0.5

0.0073

0.091

BR-10-20

342

343.8

1.8

0.0086

0.0075

0.037

0.0004

0.061

BR-10-20

343.8

345

1.2

0.0171

0.0623

0.025

0.6

0.0023

0.061

BR-10-20

345

347

2

0.0795

0.035

0.023

1.4

0.0067

0.259

BR-10-20

347

349

2

0.168

0.0828

0.007

2.7

0.0033

0.654

BR-10-20

349

351

2

0.0095

0.0013

0.6

0.0028

0.532

BR-10-20

351

353

2

0.0085

0.0008

0.0003

0.152

BR-10-20

353

355

2

0.0104

0.0007

0.0005

0.198

BR-10-20

355

357

2

0.0096

0.0014

0.8

0.0034

0.091

BR-10-20

357

359

2

0.0111

0.0015

0.6

0.0014

0.198

BR-10-20

359

361

2

0.0099

0.0014

1.4

0.0044

0.213

BR-10-20

361

363

2

0.0106

0.0012

0.0003

0.167

BR-10-20

363

365

2

0.011

0.0011

0.0005

0.122

BR-10-20

365

367

2

0.0114

0.002

3.7

0.0093

0.228

BR-10-20

367

369

2

0.0118

0.0015

1.4

0.004

0.274

BR-10-20

369

371

2

0.0124

0.0032

0.9

0.0006

0.152

BR-10-20

371

373

2

0.0117

0.0013

0.8

0.0005

0.152

BR-10-20

373

373.6

0.6

0.012

0.0051

1.2

0.0005

0.243

 

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-11-20

0

1.8

1.8

0.0263

0.019

0.01

0.0082

0.076

BR-11-20

1.8

3

1.2

0.0037

0.0015

0.0021

0.015

BR-11-20

3

5

2

0.0038

0.0015

0.0018

0.008

BR-11-20

5

6.5

1.5

No sample

BR-11-20

6.5

8.1

1.6

0.006

0.0085

0.005

0.015

BR-11-20

8.1

10

1.9

0.0297

0.263

0.005

5.5

0.024

0.046

BR-11-20

10

11.3

1.3

0.0243

0.197

0.006

1.5

0.0102

0.076

BR-11-20

11.3

12.6

1.3

0.0138

0.0059

0.0006

0.03

BR-11-20

12.6

13.5

0.9

No sample

BR-11-20

13.5

15

1.5

0.0103

0.0023

0.002

0.03

BR-11-20

15

15.7

0.7

0.011

0.0033

0.0017

0.015

BR-11-20

15.7

17

1.3

0.0121

0.0035

0.0019

0.015

BR-11-20

17

18.4

1.4

0.0122

0.0029

0.0005

0.015

BR-11-20

18.4

20

1.6

0.0075

0.0013

0.0001

0.03

BR-11-20

20

22

2

0.0122

0.0012

0.046

BR-11-20

22

24

2

0.0069

0.001

0.03

BR-11-20

24

26

2

0.0101

0.0045

0.007

0.0057

0.015

BR-11-20

26

28

2

0.0085

0.0125

0.03

BR-11-20

28

30

2

0.0101

0.0017

0.0003

0.03

BR-11-20

30

31

1

0.0099

0.0013

0.0003

0.015

BR-11-20

31

32.3

1.3

0.0093

0.0034

0.0035

0.015

BR-11-20

32.3

34

1.7

0.0107

0.0023

0.0002

0.076

BR-11-20

34

35.5

1.5

0.0113

0.0024

0.0001

0.03

BR-11-20

35.5

37

1.5

0.0121

0.0022

0.0063

0.03

BR-11-20

37

39

2

0.0172

0.0036

0.0003

0.106

BR-11-20

39

41

2

0.0147

0.0018

0.0001

0.03

BR-11-20

41

43

2

0.0129

0.002

0.061

BR-11-20

43

45

2

0.0123

0.0018

0.0009

0.046

BR-11-20

45

47

2

0.013

0.0015

0.0042

0.061

BR-11-20

47

49

2

0.0102

0.0015

0.0001

0.076

BR-11-20

49

50.2

1.2

0.0097

0.0011

0.0001

0.046

BR-11-20

50.2

52

1.8

0.0103

0.0011

0.5

0.0002

0.061

BR-11-20

52

53

1

0.018

0.0015

2

0.0017

0.137

BR-11-20

53

55

2

0.0094

0.0013

0.0004

0.122

BR-11-20

55

56.5

1.5

0.0095

0.0009

0.0002

0.076

BR-11-20

56.5

57.5

1

0.171

0.0336

0.7

0.0035

0.091

BR-11-20

57.5

58.6

1.1

0.0917

0.0184

0.008

5

0.0022

0.837

BR-11-20

58.6

59.6

1

0.137

0.0436

0.043

18

0.0087

2.115

BR-11-20

59.6

60.6

1

0.371

0.13

0.078

134

0.002

12.368

BR-11-20

60.6

61.6

1

0.15

0.0949

0.057

27.2

0.0012

5.811

BR-11-20

61.6

62.2

0.6

0.115

0.0715

0.226

10.1

0.0385

15.669

BR-11-20

62.2

63.2

1

2.22

2.86

0.596

204

0.567

75.149

BR-11-20

63.2

64.2

1

1.145

1.18

0.534

120

1.07

86.559

BR-11-20

64.2

64.8

0.6

3.09

3.42

1.925

283

0.778

83.212

BR-11-20

64.8

65.6

0.8

0.0621

0.0913

0.093

9.6

0.0362

7.454

BR-11-20

65.6

65.9

0.3

4.42

3.76

1.165

303

0.582

81.082

BR-11-20

65.9

67

1.1

1.315

0.926

0.43

118

0.133

23.883

BR-11-20

67

68

1

0.0795

0.0599

0.028

1.4

0.0193

0.593

BR-11-20

68

68.5

0.5

0.0276

0.0558

0.028

0.8

0.0075

0.228

BR-11-20

68.5

69.2

0.7

0.0255

0.0544

0.042

0.5

0.0276

0.73

BR-11-20

69.2

71

1.8

0.0041

0.0015

0.001

0.03

BR-11-20

71

73

2

0.0062

0.0017

0.002

0.015

BR-11-20

73

75

2

0.0044

0.0012

0.0008

0.03

BR-11-20

75

76

1

0.0114

0.0036

0.008

0.015

BR-11-20

76

77.3

1.3

0.0116

0.0938

0.0397

0.046

BR-11-20

77.3

79

1.7

0.0041

0.0041

0.0029

0.046

BR-11-20

79

81

2

0.0041

0.0007

0.0021

0.015

BR-11-20

81

83

2

0.0061

0.0007

0.0018

0.015

BR-11-20

83

85

2

0.0037

0.0005

0.0018

0.015

BR-11-20

85

87

2

0.0053

0.0019

0.015

BR-11-20

87

89

2

0.0074

0.0023

0.001

0.046

BR-11-20

89

91

2

0.0052

0.0017

0.006

0.001

0.03

BR-11-20

91

93

2

0.0053

0.001

0.0017

0.046

BR-11-20

93

95

2

0.0065

0.002

0.002

0.046

BR-11-20

95

97

2

0.0077

0.0048

0.0029

0.015

BR-11-20

97

99

2

0.0062

0.0038

0.0019

0.259

BR-11-20

99

100

1

0.006

0.0037

0.0021

0.03

BR-11-20

100

102

2

0.0059

0.0017

0.0011

0.015

BR-11-20

102

104

2

0.0088

0.0018

0.0009

0.015

BR-11-20

104

106

2

0.009

0.0012

0.0014

0.03

BR-11-20

106

108

2

0.0052

0.0019

0.0016

0.03

BR-11-20

108

110

2

0.008

0.0021

0.0012

0.015

BR-11-20

110

112

2

0.0104

0.0016

0.0022

0.03

BR-11-20

112

114

2

0.0078

0.002

0.0013

0.03

BR-11-20

114

116

2

0.0074

0.002

0.0009

0.243

BR-11-20

116

118

2

0.0072

0.0027

0.0017

0.015

BR-11-20

118

120

2

0.0189

0.0014

0.0011

0.183

BR-11-20

120

122

2

0.0107

0.0021

0.0013

0.03

BR-11-20

122

123.8

1.8

0.0068

0.0063

0.0021

0.046

BR-11-20

123.8

125

1.2

0.006

0.0017

0.0046

0.03

BR-11-20

125

127

2

0.009

0.0022

0.008

0.0031

0.015

BR-11-20

127

128.9

1.9

0.0336

0.0082

0.0042

0.091

BR-11-20

128.9

130.2

1.3

0.0109

0.0695

0.006

0.0055

0.578

BR-11-20

130.2

132.2

2

0.0195

0.012

0.006

0.0005

0.015

BR-11-20

132.2

134.2

2

0.0113

0.0103

0.0046

0.03

BR-11-20

134.2

135

0.8

0.0109

0.006

0.009

0.5

0.0039

0.198

BR-11-20

135

136

1

0.013

0.0106

0.5

0.0032

0.046

BR-11-20

136

137

1

0.0096

0.03

0.005

0.5

0.0054

0.076

BR-11-20

137

138

1

0.0087

0.029

0.0044

0.076

BR-11-20

138

139

1

0.0063

0.0178

0.01

0.0047

0.122

BR-11-20

139

140

1

0.01

0.0137

0.014

0.0064

0.517

BR-11-20

140

141

1

0.0141

0.0511

0.008

0.0167

0.152

BR-11-20

141

142.2

1.2

0.0216

0.0553

0.007

0.0129

0.106

BR-11-20

142.2

143

0.8

0.0246

0.0212

0.5

0.0027

0.411

BR-11-20

143

144

1

0.006

0.0032

0.0005

0.137

BR-11-20

144

145

1

0.0051

0.0033

0.0015

0.106

BR-11-20

145

146

1

0.0268

0.0051

0.0007

0.183

BR-11-20

146

146.8

0.8

0.0122

0.0047

0.0013

0.046

BR-11-20

146.8

147.3

0.5

0.0153

0.0026

0.0012

0.152

BR-11-20

147.3

148.5

1.2

0.0148

0.0021

0.007

0.0014

0.046

BR-11-20

148.5

150.5

2

0.0104

0.0017

0.0005

0.061

BR-11-20

150.5

152.5

2

0.0093

0.0029

0.0026

0.046

BR-11-20

152.5

154

1.5

0.0235

0.0103

0.002

0.03

BR-11-20

154

156

2

0.0149

0.0043

0.0019

0.046

BR-11-20

156

158

2

0.01

0.0032

0.0012

0.046

BR-11-20

158

159

1

0.0077

0.003

0.0015

0.03

BR-11-20

159

161

2

0.0119

0.0019

0.0012

0.061

BR-11-20

161

163

2

0.0128

0.0035

0.0008

0.137

BR-11-20

163

163.7

0.7

0.0146

0.0018

0.0002

0.061

BR-11-20

163.7

165.4

1.7

0.0139

0.0027

0.0031

0.106

BR-11-20

165.4

167.4

2

0.008

0.0017

0.0019

0.243

BR-11-20

167.4

169.4

2

0.0079

0.0016

0.137

BR-11-20

169.4

171

1.6

0.0077

0.0011

0.0034

0.061

BR-11-20

171

173

2

0.0068

0.001

0.0004

0.076

BR-11-20

173

175

2

0.0059

0.0007

0.0013

0.076

BR-11-20

175

177

2

0.0067

0.0009

0.0018

0.076

BR-11-20

177

179

2

0.0062

0.0012

0.0012

0.091

BR-11-20

179

181

2

0.0052

0.0012

0.005

0.0014

0.061

BR-11-20

181

182

1

0.0121

0.0058

0.017

0.0028

0.061

BR-11-20

182

183

1

0.0059

0.0036

0.013

0.0007

0.061

BR-11-20

183

184

1

0.0075

0.0009

0.005

0.0018

0.213

 

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-12-20

0

1

1

0.0099

0.0053

0.0109

0.046

BR-12-20

1

2.6

1.6

0.0095

0.0018

0.0074

0.03

BR-12-20

2.6

3.1

0.5

No sample

BR-12-20

3.1

5

1.9

0.0085

0.0021

0.005

0.0073

0.046

BR-12-20

5

7

2

0.0101

0.0018

0.006

0.0107

0.046

BR-12-20

7

9.6

2.6

No sample

BR-12-20

9.6

10.4

0.8

0.0088

0.0016

0.007

0.0058

0.03

BR-12-20

10.4

12

1.6

0.0076

0.0042

0.005

0.0038

0.046

BR-12-20

12

12.1

0.1

No sample

BR-12-20

12.1

14

1.9

0.0079

0.0044

0.005

0.0045

0.03

BR-12-20

14

17.8

3.8

No sample

BR-12-20

17.8

19.8

2

0.0069

0.002

0.006

0.0075

0.03

BR-12-20

19.8

21.5

1.7

0.0068

0.0018

0.008

0.0077

0.015

BR-12-20

21.5

24.3

2.8

No sample

BR-12-20

24.3

25.3

1

0.0056

0.0012

0.022

0.006

0.015

BR-12-20

25.3

25.8

0.5

0.0081

0.0018

0.013

0.01

0.03

BR-12-20

25.8

31

5.2

No sample

BR-12-20

31

33

2

0.0103

0.0034

0.008

0.0063

0.015

BR-12-20

33

35

2

0.0096

0.0048

0.009

0.0087

0.015

BR-12-20

35

37

2

0.0099

0.0016

0.01

0.0072

0.03

BR-12-20

37

38.6

1.6

0.008

0.0029

0.005

0.0055

0.015

BR-12-20

38.6

40

1.4

0.0038

0.0009

0.015

BR-12-20

40

41.8

1.8

0.0086

0.0017

0.0015

0.046

BR-12-20

41.8

42.6

0.8

0.0106

0.0024

0.0013

0.046

BR-12-20

42.6

45.7

3.1

No sample

BR-12-20

45.7

47.2

1.5

0.0156

0.0058

0.0015

0.076

BR-12-20

47.2

47.7

0.5

No sample

BR-12-20

47.7

49

1.3

0.0109

0.0022

0.001

0.015

BR-12-20

49

50.2

1.2

0.0067

0.0089

0.002

0.015

BR-12-20

50.2

51.4

1.2

0.002

0.0085

0.0009

0.015

BR-12-20

51.4

59.5

8.1

No sample

BR-12-20

59.5

60.7

1.2

0.0109

0.0035

0.0004

0.03

BR-12-20

60.7

62.5

1.8

0.0113

0.0062

0.0016

0.061

BR-12-20

62.5

64

1.5

0.0098

0.0009

0.0001

0.091

BR-12-20

64

66

2

0.01

0.001

0.0048

0.061

BR-12-20

66

68

2

0.0097

0.0009

0.0001

0.076

BR-12-20

68

70

2

0.0095

0.0015

0.0002

0.046

BR-12-20

70

72

2

0.0098

0.0012

0.0001

0.03

BR-12-20

72

74

2

0.0112

0.0009

0.0001

0.091

BR-12-20

74

76

2

0.0156

0.0012

0.6

0.0041

0.061

BR-12-20

76

78

2

0.017

0.0006

0.0023

0.046

BR-12-20

78

80

2

0.0161

0.0011

0.0001

0.061

BR-12-20

80

82

2

0.0164

0.0009

1.9

0.0076

0.061

BR-12-20

82

84

2

0.0162

0.0012

0.6

0.0028

0.061

BR-12-20

84

86

2

0.0127

0.0016

1.4

0.0062

0.091

BR-12-20

86

88

2

0.0092

0.0012

0.0003

0.061

BR-12-20

88

90

2

0.0086

0.0012

0.0001

0.03

BR-12-20

90

92

2

0.0079

0.0013

0.0001

0.046

BR-12-20

92

94

2

0.009

0.001

0.0008

0.061

BR-12-20

94

96

2

0.0127

0.001

0.0006

0.122

BR-12-20

96

98

2

0.01

0.0013

0.0001

0.046

BR-12-20

98

100

2

0.0115

0.0014

0.0001

0.076

BR-12-20

100

102

2

0.0123

0.001

2.8

0.0027

0.167

BR-12-20

102

102.7

0.7

0.0142

0.0012

13.6

0.0134

0.091

BR-12-20

102.7

103.5

0.8

0.208

0.0242

0.005

6.4

0.0041

1.978

BR-12-20

103.5

104.5

1

0.1805

0.0276

0.033

14.6

0.0016

3.24

BR-12-20

104.5

105.5

1

0.511

0.257

0.037

13.9

0.0059

1.217

BR-12-20

105.5

106.5

1

0.0863

0.0153

0.013

1.1

0.0028

0.38

BR-12-20

106.5

107.5

1

0.0578

0.0113

0.009

2.1

0.0029

2.54

BR-12-20

107.5

108.5

1

0.047

0.0089

3.9

0.0006

0.867

BR-12-20

108.5

109

0.5

0.1425

0.103

0.006

65.7

0.0061

0.35

BR-12-20

109

109.7

0.7

0.1685

0.0647

0.009

34.6

0.0034

0.335

BR-12-20

109.7

110.5

0.8

0.0117

0.011

0.028

1.9

0.0018

1.46

BR-12-20

110.5

111.5

1

0.1185

0.446

0.059

8.4

0.0491

3.499

BR-12-20

111.5

112.5

1

0.376

0.165

0.2

6.8

0.0213

3.636

BR-12-20

112.5

113.5

1

0.683

0.339

0.3

31

0.131

6.587

BR-12-20

113.5

114

0.5

4.75

3.78

1.455

220

0.549

70.89

BR-12-20

114

114.7

0.7

11.6

6.39

2.56

520

0.59

69.216

BR-12-20

114.7

116.4

1.7

1.53

2.12

0.717

104

0.0878

4.822

BR-12-20

116.4

118.4

2

0.016

0.0174

0.005

0.0038

0.563

BR-12-20

118.4

118.9

0.5

No sample

BR-12-20

118.9

120.8

1.9

0.0755

0.0649

0.005

0.0077

0.152

BR-12-20

120.8

122.8

2

0.0239

0.0157

0.01

0.0177

0.046

BR-12-20

122.8

124.5

1.7

0.0063

0.0035

0.0014

0.046

BR-12-20

124.5

126.5

2

0.0075

0.003

0.0015

0.03

BR-12-20

126.5

128.5

2

0.0091

0.0038

0.005

0.0018

0.03

BR-12-20

128.5

130.1

1.6

0.0096

0.0036

0.0013

0.03

 

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-13-20

0

1.5

1.5

0.0095

0.0024

0.006

0.0074

0.061

BR-13-20

1.5

4.8

3.3

No sample

BR-13-20

4.8

6.7

1.9

0.0094

0.0021

0.005

0.0053

0.046

BR-13-20

6.7

8.2

1.5

0.0105

0.0027

0.0066

0.046

BR-13-20

8.2

10.2

2

0.0097

0.0014

0.0066

0.046

BR-13-20

10.2

12.2

2

0.0099

0.0017

0.005

0.0064

0.046

BR-13-20

12.2

14.2

2

0.0113

0.0026

0.006

0.0077

0.091

BR-13-20

14.2

16.2

2

0.0073

0.002

0.007

0.03

BR-13-20

16.2

18.2

2

0.0085

0.0019

0.007

0.0047

0.046

BR-13-20

18.2

19.8

1.6

0.0031

0.0013

0.0016

0.015

BR-13-20

19.8

21.8

2

0.0035

0.001

0.0018

0.015

BR-13-20

21.8

23.7

1.9

0.0066

0.0013

0.005

0.0062

0.015

BR-13-20

23.7

25.7

2

0.0067

0.0023

0.006

0.005

0.015

BR-13-20

25.7

27.2

1.5

0.0169

0.0204

0.01

0.0089

0.03

BR-13-20

27.2

28.2

1

0.0284

0.0559

0.015

0.0119

0.03

BR-13-20

28.2

30

1.8

0.0113

0.0078

0.012

0.0103

0.091

BR-13-20

30

32

2

0.007

0.0024

0.009

0.007

0.015

BR-13-20

32

34

2

0.0084

0.0022

0.009

0.0076

0.03

BR-13-20

34

36

2

0.0104

0.0023

0.017

0.0079

0.03

BR-13-20

36

38

2

0.0075

0.0026

0.011

0.0066

0.015

BR-13-20

38

40

2

0.0084

0.0022

0.0049

0.03

BR-13-20

40

42

2

0.0056

0.002

0.0036

0.061

BR-13-20

42

44

2

0.0089

0.0038

0.0058

0.03

BR-13-20

44

44.9

0.9

0.0095

0.0075

0.0027

0.015

BR-13-20

44.9

46.9

2

0.0064

0.0039

0.0015

0.03

BR-13-20

46.9

48.3

1.4

0.0067

0.0054

0.001

0.03

BR-13-20

48.3

49.5

1.2

0.0099

0.0022

0.0009

0.015

BR-13-20

49.5

50.6

1.1

0.015

0.0027

0.0015

0.015

BR-13-20

50.6

52.6

2

0.007

0.0009

0.0013

0.03

BR-13-20

52.6

54.6

2

0.0114

0.0018

0.0009

0.015

BR-13-20

54.6

56.6

2

0.0138

0.005

0.006

0.0029

0.03

BR-13-20

56.6

57.3

0.7

0.0119

0.0017

0.0012

0.046

BR-13-20

57.3

59

1.7

0.0105

0.0011

0.0012

0.061

BR-13-20

59

60.5

1.5

0.0129

0.002

0.0036

0.046

BR-13-20

60.5

62.5

2

0.0118

0.003

0.0015

0.046

BR-13-20

62.5

64.5

2

0.0138

0.0019

0.0044

0.061

BR-13-20

64.5

66.5

2

0.0121

0.0009

0.0011

0.152

BR-13-20

66.5

68.5

2

0.0182

0.0088

4.4

0.0033

0.243

BR-13-20

68.5

70

1.5

0.0108

0.0013

0.8

0.0006

0.502

BR-13-20

70

70.9

0.9

0.0101

0.0014

0.9

0.0013

0.046

BR-13-20

70.9

72

1.1

0.0067

0.0058

3

0.0021

0.122

BR-13-20

72

74

2

0.0114

0.0014

1.7

0.0019

0.122

BR-13-20

74

76

2

0.0086

0.0163

5.4

0.0018

0.624

BR-13-20

76

77

1

0.0054

0.0036

1.1

0.0008

0.289

BR-13-20

77

78.1

1.1

0.0064

0.0024

5.1

0.002

0.228

BR-13-20

78.1

80

1.9

0.0084

0.0008

0.007

16.6

0.0036

0.304

BR-13-20

80

82

2

0.0153

0.0041

0.006

5.4

0.0015

0.502

BR-13-20

82

84

2

0.0173

0.0067

23

0.0048

0.213

BR-13-20

84

86

2

0.0105

0.0015

2.2

0.0008

0.639

BR-13-20

86

87

1

0.0099

0.0009

0.0005

0.456

BR-13-20

87

88.4

1.4

0.0091

0.0012

1

0.001

1.293

BR-13-20

88.4

90

1.6

0.0092

0.0035

2.4

0.0014

0.167

BR-13-20

90

92

2

0.0072

0.0033

3.1

0.0022

0.122

BR-13-20

92

94

2

0.0098

0.0009

0.5

0.0004

0.243

BR-13-20

94

96

2

0.0091

0.0013

2

0.0014

1.947

BR-13-20

96

96.8

0.8

0.0455

0.0185

8.3

0.0029

2.54

BR-13-20

96.8

98

1.2

0.0123

0.0066

3.3

0.0015

0.441

BR-13-20

98

99.1

1.1

0.0205

0.0096

9.3

0.0023

0.183

BR-13-20

99.1

100.6

1.5

0.0291

0.0167

26.6

0.0058

1.323

BR-13-20

100.6

102.1

1.5

0.0117

0.0064

3.4

0.003

0.183

BR-13-20

102.1

104

1.9

0.0139

0.0013

0.0001

0.091

BR-13-20

104

106

2

0.0142

0.0013

2.3

0.004

0.076

BR-13-20

106

108

2

0.0154

0.0012

0.0004

0.456

BR-13-20

108

110

2

0.0111

0.0011

0.0001

0.122

BR-13-20

110

112

2

0.01

0.0009

0.0002

0.183

BR-13-20

112

114

2

0.0096

0.0021

2.2

0.0014

0.106

BR-13-20

114

116

2

0.0278

0.0159

11.3

0.0107

0.624

BR-13-20

116

118

2

0.0198

0.0038

2.3

0.003

0.167

BR-13-20

118

120

2

0.0091

0.0014

2.2

0.0007

0.304

BR-13-20

120

121.65

1.65

0.0104

0.0035

0.009

3.5

0.0002

0.243

BR-13-20

121.65

122.5

0.85

0.125

0.0482

0.044

22.1

0.0033

2.343

BR-13-20

122.5

123.5

1

0.371

0.143

0.085

35.7

0.0067

3.134

BR-13-20

123.5

124.5

1

1.275

1.495

0.172

33.3

1.384

BR-13-20

124.5

125.5

1

1.08

0.325

0.263

18.8

0.797

4.168

BR-13-20

125.5

126.5

1

1.28

0.377

0.532

23.5

1.105

0.882

BR-13-20

126.5

127

0.5

0.209

0.0229

0.296

2

0.0154

0.106

BR-13-20

127

127.5

0.5

0.1685

0.0049

0.076

0.5

0.002

0.532

BR-13-20

127.5

128.5

1

0.824

0.66

0.188

15.4

0.267

2.83

BR-13-20

128.5

129.5

1

12

8.32

1.29

160

2.02

1.171

BR-13-20

129.5

130.5

1

5.49

2.84

0.751

69.4

0.491

7.013

BR-13-20

130.5

131.5

1

0.65

0.502

0.36

25.3

0.116

6.648

BR-13-20

131.5

132.6

1.1

0.935

0.398

0.325

55

0.157

13.113

BR-13-20

132.6

133.7

1.1

1.075

0.392

0.21

22.5

0.29

15.441

BR-13-20

133.7

134

0.3

1.665

2.13

2.27

106

0.51

84.429

BR-13-20

134

134.9

0.9

1.905

2.23

3.18

174

0.584

84.277

BR-13-20

134.9

136

1.1

0.174

0.226

0.196

9.2

0.016

7.606

BR-13-20

136

137

1

0.287

0.176

0.028

11.3

0.0124

0.654

BR-13-20

137

138

1

0.286

0.101

0.014

10.3

0.0106

0.03

BR-13-20

138

139.1

1.1

0.37

0.26

0.012

9.4

0.0078

1.582

BR-13-20

139.1

141

1.9

0.0732

0.132

0.007

1

0.0039

1.171

BR-13-20

141

143

2

0.144

0.022

0.009

0.0068

0.076

BR-13-20

143

145

2

0.0529

0.0265

0.018

0.0093

0.03

BR-13-20

145

147

2

0.0128

0.0322

0.023

0.012

0.061

BR-13-20

147

149

2

0.0265

0.0362

0.024

0.008

0.03

BR-13-20

149

149.5

0.5

No sample

BR-13-20

149.5

151.5

2

0.0229

0.0115

0.0035

0.03

BR-13-20

151.5

153.5

2

0.005

0.006

0.0017

0.03

BR-13-20

153.5

155.2

1.7

0.0083

0.0081

0.0007

0.03

 

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-17-20

0

118.8

No sample

BR-17-20

118.8

119.8

1

0.261

0.342

0.017

2.6

0.026

0.213

BR-17-20

119.8

120.8

1

0.161

0.0628

3

0.0046

0.015

BR-17-20

120.8

121.8

1

0.0132

0.0056

0.0004

0.015

BR-17-20

121.8

122.8

1

0.0247

0.0081

0.0009

0.015

BR-17-20

122.8

123.8

1

0.0276

0.0037

0.006

0.0004

0.03

BR-17-20

123.8

124.8

1

0.0074

0.0017

0.0001

0.008

BR-17-20

124.8

125.8

1

0.0052

0.0016

0.0004

0.008

BR-17-20

125.8

126.5

0.7

0.343

0.0791

0.005

1.1

0.0035

0.015

BR-17-20

126.5

127

0.5

0.369

0.104

0.008

5.6

0.0074

0.015

BR-17-20

127

127.5

0.5

0.257

0.0508

0.006

6.8

0.0058

0.015

BR-17-20

127.5

128

0.5

0.123

0.0312

0.008

1.2

0.0021

0.015

BR-17-20

128

128.5

0.5

0.287

0.0628

0.007

0.003

0.015

BR-17-20

128.5

129

0.5

0.102

0.159

0.009

4.9

0.0052

0.015

BR-17-20

129

129.5

0.5

0.138

0.0238

2.6

0.0031

0.008

BR-17-20

129.5

130.5

1

0.029

0.0062

0.005

0.5

0.0003

0.008

BR-17-20

130.5

131

0.5

0.0371

0.0329

1

0.001

0.008

BR-17-20

131

132

1

0.0424

0.0646

0.006

0.9

0.0009

0.008

BR-17-20

132

133

1

0.0754

0.0806

0.013

0.9

0.0007

0.008

BR-17-20

133

133.5

0.5

0.019

0.0444

0.007

0.8

0.0006

0.008

BR-17-20

133.5

134

0.5

0.0151

0.0501

0.0005

0.008

BR-17-20

134

134.5

0.5

0.0074

0.0157

0.005

0.0001

0.008

BR-17-20

134.5

135

0.5

0.0029

0.0096

0.0005

0.008

BR-17-20

135

136

1

0.0055

0.0086

0.0003

0.008

BR-17-20

136

137

1

0.0029

0.0106

0.0003

0.008

BR-17-20

137

138

1

0.0138

0.0073

0.0002

0.008

BR-17-20

138

139

1

0.02

0.0084

0.005

0.0001

0.008

BR-17-20

139

140

1

0.0226

0.0105

0.0001

0.008

BR-17-20

140

141

1

0.0064

0.0079

0.038

0.0001

0.015

BR-17-20

141

142

1

0.022

0.0449

0.02

1.4

0.0007

0.008

BR-17-20

142

143

1

0.0199

0.0464

0.5

0.0004

0.008

BR-17-20

143

144

1

0.0205

0.0842

0.0003

0.008

BR-17-20

144

145

1

0.0156

0.0529

0.0004

0.008

BR-17-20

145

146

1

0.0159

0.12

0.5

0.0003

0.008

BR-17-20

146

147

1

0.0181

0.0711

0.0003

0.008

BR-17-20

147

148

1

0.011

0.0497

0.0002

0.015

BR-17-20

148

149

1

0.0132

0.12

0.6

0.0004

0.076

BR-17-20

149

150

1

0.0039

0.1

0.0001

0.03

BR-17-20

150

151

1

0.0141

0.295

1.1

0.0003

0.015

BR-17-20

151

152

1

0.0037

0.0534

0.006

0.0002

0.015

BR-17-20

152

153

1

0.0273

0.026

0.0002

0.03

BR-17-20

153

154

1

0.0071

0.0058

0.005

0.0001

0.008

BR-17-20

154

155

1

0.0033

0.0037

0.006

0.0003

0.008

BR-17-20

155

156

1

0.0022

0.0011

0.0006

0.03

BR-17-20

156

157

1

0.0004

0.0002

0.106

BR-17-20

157

158

1

0.0033

0.0004

0.005

0.0001

0.076

BR-17-20

158

159

1

0.0041

0.0018

0.0016

0.03

BR-17-20

159

160

1

0.0084

0.0012

0.0003

0.015

BR-17-20

160

161

1

0.0086

0.0026

0.001

0.015

BR-17-20

161

162

1

0.0052

0.002

0.0021

0.03

BR-17-20

162

163

1

0.0038

0.0019

0.0007

0.015

BR-17-20

163

163.6

0.6

0.0028

0.0009

0.005

0.0006

0.015

BR-17-20

163.6

164.5

0.9

0.012

0.0037

0.0038

0.03

BR-17-20

164.5

165.5

1

0.0106

0.0018

0.002

0.061

BR-17-20

165.5

166.5

1

0.01

0.002

0.0012

0.076

BR-17-20

166.5

167.5

1

0.0147

0.0036

0.0022

0.091

BR-17-20

167.5

168

0.5

0.0219

0.0124

0.013

0.061

BR-17-20

168

168.9

0.9

0.0134

0.0035

0.0013

0.061

BR-17-20

168.9

170.8

1.9

0.0123

0.005

0.0004

0.046

BR-17-20

170.8

172.8

2

0.0128

0.0021

0.0004

0.046

BR-17-20

172.8

174.8

2

0.0087

0.0065

0.0039

0.076

BR-17-20

174.8

176

1.2

0.0104

0.0016

0.0003

0.076

BR-17-20

176

178

2

0.0136

0.001

0.002

0.061

BR-17-20

178

179

1

0.013

0.0013

0.0002

0.03

BR-17-20

179

180.1

1.1

0.0134

0.001

0.0056

0.061

BR-17-20

180.1

182.1

2

0.0197

0.007

0.0015

0.73

BR-17-20

182.1

183

0.9

0.0398

0.0114

0.0022

0.061

BR-17-20

183

184

1

0.009

0.0033

0.002

0.411

BR-17-20

184

185

1

0.0099

0.0023

0.9

0.0009

0.472

BR-17-20

185

186

1

0.0121

0.0073

0.011

1.7

0.0019

0.335

BR-17-20

186

187

1

0.0697

0.0267

0.015

19

0.0064

0.396

BR-17-20

187

188

1

0.013

0.0016

0.01

0.7

0.0004

0.198

BR-17-20

188

189

1

0.0149

0.0042

0.008

3.5

0.0017

0.548

BR-17-20

189

190

1

0.0092

0.0063

0.006

4.9

0.0011

0.806

BR-17-20

190

191

1

0.0219

0.017

0.021

6.7

0.0019

1.019

BR-17-20

191

192

1

0.38

0.261

0.027

49.6

0.0147

2.83

BR-17-20

192

192.9

0.9

0.0161

0.0252

0.018

4.2

0.0016

2.221

BR-17-20

192.9

193.5

0.6

1.67

0.288

0.966

279

0.585

36.206

BR-17-20

193.5

194

0.5

4.13

2.81

1.75

137

1.29

54.46

BR-17-20

194

194.5

0.5

2.23

0.754

2.01

124

0.324

38.944

BR-17-20

194.5

195

0.5

0.606

0.221

0.692

19.3

0.0881

11.546

BR-17-20

195

196

1

0.229

0.0482

0.157

4.5

0.0239

1.034

BR-17-20

196

196.5

0.5

0.226

0.0879

0.151

4

0.0407

3.59

BR-17-20

196.5

197

0.5

0.0818

0.0327

0.227

6.7

0.0211

0.578

BR-17-20

197

198

1

0.0633

0.0098

0.095

2.4

0.0058

0.532

BR-17-20

198

199

1

0.0993

0.0126

0.084

1.2

0.0035

0.106

BR-17-20

199

200

1

0.0483

0.0233

0.082

1.2

0.0047

0.061

BR-17-20

200

201

1

0.0182

0.0104

0.062

1.1

0.0021

0.046

BR-17-20

201

202

1

0.0127

0.0034

0.021

0.001

0.03

BR-17-20

202

203

1

0.0333

0.0157

0.069

0.9

0.0065

0.806

BR-17-20

203

203.5

0.5

0.105

0.0455

0.077

0.9

0.0129

0.274

BR-17-20

203.5

204

0.5

0.043

0.0089

0.056

0.0023

0.487

BR-17-20

204

204.5

0.5

1.315

0.414

0.883

112

0.235

19.852

BR-17-20

204.5

205

0.5

1.135

0.493

0.774

151

0.249

31.642

BR-17-20

205

205.5

0.5

0.734

0.322

0.682

79.2

0.0916

15.288

BR-17-20

205.5

206

0.5

4.21

2.05

1.21

223

0.506

36.966

BR-17-20

206

206.7

0.7

0.21

0.372

0.532

42.3

0.0483

4.503

BR-17-20

206.7

208

1.3

0.0053

0.0019

0.006

0.001

0.076

BR-17-20

208

210

2

0.0039

0.0008

0.016

0.0037

0.015

BR-17-20

210

212

2

0.0037

0.0008

0.0023

0.015

BR-17-20

212

214

2

0.0057

0.002

0.0024

0.03

BR-17-20

214

216

2

0.006

0.0017

0.01

0.0018

0.015

BR-17-20

216

218

2

0.0036

0.0016

0.005

0.0012

0.03

BR-17-20

218

220

2

0.0062

0.0017

0.0015

0.091

BR-17-20

220

222

2

0.008

0.0028

0.0512

0.106

BR-17-20

222

222.9

0.9

0.0123

0.0034

0.012

0.0066

0.441

BR-17-20

222.9

223.5

0.6

0.243

0.302

0.028

1.1

0.031

1.308

BR-17-20

223.5

224

0.5

0.31

0.226

0.063

1.5

0.0259

1.354

BR-17-20

224

224.5

0.5

0.207

0.172

0.05

0.8

0.0246

0.73

BR-17-20

224.5

225

0.5

0.204

0.0557

0.038

1.1

0.0182

0.426

BR-17-20

225

225.5

0.5

0.0601

0.0244

0.033

1.8

0.0256

0.213

BR-17-20

225.5

226

0.5

0.0103

0.013

0.02

0.7

0.0091

0.517

BR-17-20

226

226.5

0.5

0.0164

0.012

0.01

0.6

0.0047

0.472

BR-17-20

226.5

227.2

0.7

0.0194

0.0654

0.015

0.6

0.0095

1.034

BR-17-20

227.2

228.9

1.7

0.0098

0.0063

0.007

0.0164

0.761

BR-17-20

228.9

229.7

0.8

0.0701

0.15

0.03

0.6

0.025

11.637

BR-17-20

229.7

230.5

0.8

0.0823

0.231

0.231

9.1

0.0252

9.371

BR-17-20

230.5

231

0.5

8.63

6.12

3.12

341

0.334

38.335

BR-17-20

231

231.5

0.5

5.67

4.11

1.74

266

0.492

13.737

BR-17-20

231.5

232

0.5

1.515

2.26

1.36

67.4

0.383

7.226

BR-17-20

232

232.9

0.9

0.177

0.409

0.515

8.1

0.11

4.716

BR-17-20

232.9

234

1.1

0.0107

0.0149

0.052

13.3

0.0093

0.821

BR-17-20

234

235

1

0.0494

0.0177

0.054

18.1

0.003

1.156

BR-17-20

235

236

1

0.0829

0.0406

0.063

4.5

0.0015

BR-17-20

236

237

1

0.0501

0.0315

0.036

3.2

0.0105

1.308

BR-17-20

237

237.8

0.8

0.278

0.0564

0.139

2.1

0.007

0.061

BR-17-20

237.8

238.8

1

0.266

0.453

0.396

22.2

0.0264

0.091

BR-17-20

238.8

239.8

1

0.502

0.213

0.14

9.5

0.013

0.061

BR-17-20

239.8

240.8

1

0.182

0.121

0.153

15.7

0.0299

0.03

BR-17-20

240.8

241.8

1

0.0401

0.013

0.104

5.1

0.0023

0.046

BR-17-20

241.8

242.5

0.7

0.127

0.0363

0.124

9.3

0.0046

0.046

BR-17-20

242.5

243

0.5

0.188

0.0829

0.137

10.2

0.0087

0.046

BR-17-20

243

243.5

0.5

0.417

0.43

0.207

140

0.0319

0.289

BR-17-20

243.5

244

0.5

0.225

0.141

0.189

130

0.0366

0.167

BR-17-20

244

244.5

0.5

0.719

0.349

0.233

124

0.0361

0.791

BR-17-20

244.5

245

0.5

1.05

0.498

0.313

262

0.0839

1.719

BR-17-20

245

245.5

0.5

0.203

0.0423

0.127

8.7

0.0026

0.152

BR-17-20

245.5

246

0.5

0.118

0.067

0.182

7.2

0.0037

0.106

BR-17-20

246

246.5

0.5

0.694

0.264

0.459

29

0.0174

2.297

BR-17-20

246.5

247

0.5

0.892

0.512

0.457

41.1

0.0229

1.004

BR-17-20

247

247.5

0.5

1.11

0.541

0.388

84.1

0.0446

1.491

BR-17-20

247.5

248

0.5

1.07

0.341

0.372

48.9

0.0291

0.791

BR-17-20

248

248.5

0.5

0.872

0.383

0.548

49.6

0.0354

0.259

BR-17-20

248.5

249

0.5

0.253

0.1005

0.423

12

0.0102

0.274

BR-17-20

249

249.5

0.5

0.595

0.1215

0.464

14.3

0.015

0.502

BR-17-20

249.5

250

0.5

1.415

0.699

0.42

49.7

0.0408

1.05

BR-17-20

250

250.5

0.5

2.11

0.855

0.427

79.1

0.0779

1.536

BR-17-20

250.5

251

0.5

0.852

0.404

0.462

25.8

0.0364

0.624

BR-17-20

251

252

1

0.97

0.53

0.498

32.6

0.0446

0.852

BR-17-20

252

253

1

0.568

0.319

0.295

13.2

0.022

0.898

BR-17-20

253

254

1

0.411

0.285

0.355

8.4

0.0245

0.7

BR-17-20

254

255

1

0.191

0.352

0.242

17.3

0.0233

0.837

BR-17-20

255

256

1

0.0438

0.672

0.338

29.7

0.0299

0.38

BR-17-20

256

257

1

0.735

0.426

0.275

19.9

0.0211

0.304

BR-17-20

257

258

1

0.325

0.146

0.267

4.2

0.0084

0.73

BR-17-20

258

259

1

0.125

0.0665

0.423

3.8

0.0056

0.076

BR-17-20

259

260

1

0.335

0.18

0.282

7

0.0241

0.076

BR-17-20

260

261

1

0.33

0.152

0.304

4.7

0.0108

0.046

BR-17-20

261

262

1

0.154

0.279

0.303

23.6

0.0642

0.365

BR-17-20

262

263

1

0.266

0.409

0.223

23.6

0.0378

0.198

BR-17-20

263

264

1

0.507

0.325

0.218

33.4

0.0493

0.213

BR-17-20

264

265

1

0.438

0.0966

0.145

4.1

0.0032

0.061

BR-17-20

265

266

1

0.219

0.218

0.138

17.1

0.023

0.137

BR-17-20

266

267

1

0.0992

0.165

0.163

12.7

0.0095

0.03

BR-17-20

267

268

1

0.185

0.0899

0.201

15

0.013

0.091

BR-17-20

268

269

1

0.429

0.206

0.233

21.6

0.0287

0.198

BR-17-20

269

270

1

2.93

1.61

0.537

137

0.202

0.791

BR-17-20

270

271

1

0.967

0.414

0.32

47.2

0.0566

0.167

BR-17-20

271

272

1

0.0682

0.0391

0.156

6.1

0.0071

0.106

BR-17-20

272

273

1

0.462

0.246

0.161

27.7

0.021

0.122

BR-17-20

273

274.2

1.2

0.201

0.284

7.1

0.006

0.122

BR-17-20

274.2

274.4

0.2

No sample

BR-17-20

274.4

275

0.6

0.381

0.1405

0.081

5.9

0.0093

0.046

BR-17-20

275

276

1

0.144

0.05

0.041

1.1

0.0033

0.03

BR-17-20

276

277

1

0.234

0.078

0.057

6.6

0.0209

0.03

BR-17-20

277

278

1

0.241

0.0252

0.069

1.8

0.0051

0.03

BR-17-20

278

279

1

0.129

0.0637

0.086

1.2

0.0041

0.046

BR-17-20

279

280

1

0.0951

0.0139

0.05

0.8

0.046

BR-17-20

280

281

1

0.0182

0.0105

0.039

0.0017

0.046

BR-17-20

281

282

1

0.007

0.0114

0.06

0.0013

0.198

BR-17-20

282

283

1

0.0066

0.0077

0.092

0.002

0.061

BR-17-20

283

284

1

0.044

0.0295

0.104

2.1

0.0048

0.122

BR-17-20

284

285

1

0.31

0.252

0.086

21.5

0.0463

0.913

BR-17-20

285

286

1

0.424

0.174

0.064

14.8

0.0328

0.152

BR-17-20

286

287

1

0.0459

0.0091

0.075

3.2

0.0106

0.046

BR-17-20

287

288

1

0.0619

0.0395

0.047

2.3

0.0084

0.046

BR-17-20

288

289

1

0.064

0.0183

0.028

8.7

0.0364

0.106

BR-17-20

289

290

1

0.264

0.141

0.044

1.4

0.0115

0.259

BR-17-20

290

291

1

0.256

0.137

0.067

2.3

0.0131

0.639

BR-17-20

291

292

1

3.03

1.3

0.088

17.2

0.306

1.673

BR-17-20

292

293

1

0.199

0.0562

0.075

1

0.0037

0.106

BR-17-20

293

293.5

0.5

0.157

0.0691

0.073

2.4

0.013

0.106

BR-17-20

293.5

294.4

0.9

0.112

0.0575

0.049

0.9

0.0035

0.046

BR-17-20

294.4

295.4

1

0.104

0.0368

0.052

0.5

0.0019

0.319

BR-17-20

295.4

296

0.6

0.0203

0.0077

0.055

0.0016

0.046

BR-17-20

296

297

1

0.0467

0.0086

0.065

0.0019

0.198

BR-17-20

297

298

1

0.246

0.0573

0.05

2.6

0.0343

1.415

BR-17-20

298

299

1

0.0581

0.0049

0.042

0.0012

0.03

BR-17-20

299

300

1

0.591

0.307

0.078

17

0.103

0.502

BR-17-20

300

301

1

0.267

0.068

0.214

4.1

0.0101

0.35

BR-17-20

301

302

1

0.0201

0.0038

0.042

0.0012

0.259

BR-17-20

302

303

1

0.0578

0.0036

0.043

0.0013

0.046

BR-17-20

303

304

1

0.0327

0.0038

0.038

0.004

0.076

BR-17-20

304

305

1

0.129

0.219

0.033

3.5

0.044

0.776

BR-17-20

305

306

1

0.0431

0.0033

0.026

0.0008

0.426

BR-17-20

306

307

1

0.148

0.0587

0.04

0.6

0.0069

0.289

BR-17-20

307

308

1

0.0937

0.0183

0.04

0.0017

0.167

BR-17-20

308

309

1

0.0359

0.0112

0.041

0.0011

0.076

BR-17-20

309

310

1

0.0228

0.0038

0.019

0.0008

0.122

BR-17-20

310

311

1

0.0355

0.0073

0.025

0.0015

0.076

BR-17-20

311

312

1

0.132

0.0169

0.043

0.0011

0.106

BR-17-20

312

313

1

0.113

0.0153

0.031

0.0015

0.319

BR-17-20

313

314

1

0.22

0.0415

0.038

0.0013

0.091

BR-17-20

314

314.7

0.7

0.0801

0.0146

0.039

0.0009

0.091

BR-17-20

314.7

315.5

0.8

0.0291

0.005

0.018

0.0006

0.046

BR-17-20

315.5

316

0.5

0.0263

0.0031

0.016

0.0005

0.03

BR-17-20

316

317

1

0.0179

0.0071

0.025

0.0006

0.03

BR-17-20

317

318

1

0.0186

0.0035

0.028

0.0007

0.03

BR-17-20

318

319

1

0.0352

0.0051

0.022

0.0007

0.03

BR-17-20

319

320

1

0.0622

0.0027

0.016

0.0007

0.137

BR-17-20

320

321

1

0.074

0.144

0.024

1.3

0.001

0.106

BR-17-20

321

322

1

0.0415

0.0149

0.01

0.0007

0.913

BR-17-20

322

323

1

0.0337

0.024

0.01

0.0005

0.137

BR-17-20

323

324

1

0.0235

0.0019

0.011

0.0005

0.091

BR-17-20

324

325

1

0.0139

0.0023

0.008

0.0003

0.046

BR-17-20

325

326

1

0.0112

0.0047

0.014

0.0005

0.046

BR-17-20

326

327

1

0.0061

0.002

0.009

0.0004

0.061

BR-17-20

327

328

1

0.0295

0.0023

0.006

0.0003

0.122

BR-17-20

328

329

1

0.0201

0.0017

0.012

0.0006

0.061

BR-17-20

329

330

1

0.0269

0.0043

0.025

0.0013

0.046

BR-17-20

330

331

1

0.0317

0.0018

0.014

0.0004

0.046

BR-17-20

331

332

1

0.0213

0.0031

0.009

0.0003

0.091

BR-17-20

332

333

1

0.024

0.0031

0.015

0.0003

0.061

BR-17-20

333

334

1

0.0694

0.006

0.012

0.0002

0.046

BR-17-20

334

335

1

0.0144

0.0019

0.007

0.0002

0.091

BR-17-20

335

336

1

0.032

0.0168

0.023

0.0009

0.167

BR-17-20

336

337

1

0.023

0.0092

0.02

0.0006

0.122

BR-17-20

337

338

1

0.2

0.085

0.038

1.1

0.0134

1.552

BR-17-20

338

339

1

0.244

0.0795

0.033

1.1

0.0172

0.274

BR-17-20

339

340

1

0.813

0.32

0.034

3.5

0.0535

0.502

BR-17-20

340

341

1

0.118

0.0133

0.021

0.0024

0.061

BR-17-20

341

342

1

0.495

0.155

0.078

4.1

0.0187

1.187

BR-17-20

342

343

1

0.364

0.0429

0.033

0.8

0.0023

2.434

BR-17-20

343

344

1

0.0578

0.0095

0.019

0.0009

0.487

BR-17-20

344

345

1

0.0552

0.0114

0.013

0.0009

0.106

BR-17-20

345

346.2

1.2

0.0908

0.0255

0.033

0.9

0.003

0.365

BR-17-20

346.2

347.4

1.2

0.177

0.0524

0.029

1.5

0.0069

0.106

BR-17-20

347.4

348.5

1.1

0.0864

0.0168

0.019

0.8

0.0016

0.35

BR-17-20

348.5

349.5

1

0.0385

0.0081

0.017

0.6

0.0009

0.091

BR-17-20

349.5

350.5

1

0.0463

0.0047

0.015

0.8

0.0005

0.304

BR-17-20

350.5

351.5

1

0.0079

0.0046

0.016

0.8

0.0009

0.228

BR-17-20

351.5

352.5

1

0.0206

0.0082

0.02

2.2

0.0007

0.106

BR-17-20

352.5

353.5

1

0.0149

0.0081

0.017

1.8

0.001

0.046

BR-17-20

353.5

354.5

1

0.194

0.168

0.027

10.2

0.0011

0.046

BR-17-20

354.5

355.5

1

0.106

0.0639

0.025

11.5

0.0011

0.122

BR-17-20

355.5

356.5

1

0.0183

0.0133

0.023

4.1

0.0018

0.046

BR-17-20

356.5

357.5

1

0.0055

0.003

0.018

4

0.0005

0.03

BR-17-20

357.5

358.5

1

0.0923

0.0242

0.019

4.7

0.0007

0.03

BR-17-20

358.5

359.5

1

0.0309

0.0122

0.017

4.3

0.0005

0.03

BR-17-20

359.5

360.5

1

0.0431

0.0102

0.019

4.7

0.0006

0.046

BR-17-20

360.5

361.5

1

0.0157

0.0072

0.017

13

0.0011

0.243

BR-17-20

361.5

363

1.5

0.0617

0.0308

0.016

8.6

0.0015

0.228

BR-17-20

363

364

1

0.0433

0.0423

0.008

4.6

0.0004

0.821

BR-17-20

364

365

1

0.114

0.0591

0.007

9.4

0.0015

0.776

BR-17-20

365

366

1

0.0325

0.0148

2.9

0.0003

0.289

BR-17-20

366

367

1

0.0172

0.0308

0.013

2.3

0.0004

0.076

BR-17-20

367

368

1

0.0379

0.0034

0.008

1.9

0.0002

0.198

BR-17-20

368

369

1

0.0613

0.0084

0.007

2.7

0.0004

0.517

BR-17-20

369

370

1

0.147

0.0272

0.005

3.6

0.0005

0.456

BR-17-20

370

371

1

0.107

0.0073

0.007

2.3

0.0004

0.152

BR-17-20

371

372

1

0.0884

0.0033

0.008

1.5

0.0002

0.35

BR-17-20

372

373

1

0.057

0.0124

0.009

1.6

0.0003

0.106

BR-17-20

373

374

1

0.0053

0.0041

0.007

2.7

0.0004

0.365

BR-17-20

374

375

1

0.0244

0.0091

0.005

1.4

0.0002

0.061

BR-17-20

375

376

1

0.0245

0.0044

1.1

0.0003

0.061

BR-17-20

376

377

1

0.0108

0.002

0.006

1.1

0.0003

0.046

BR-17-20

377

378

1

0.0197

0.0047

1

0.0003

0.091

BR-17-20

378

379

1

0.0392

0.0076

0.005

1.3

0.0004

0.228

BR-17-20

379

380

1

0.0191

0.0056

0.005

0.8

0.0004

0.076

BR-17-20

380

381

1

0.0762

0.031

0.005

1.4

0.0032

0.076

BR-17-20

381

382

1

0.0544

0.0113

0.006

0.6

0.0009

0.228

BR-17-20

382

383

1

0.187

0.0575

0.009

4.3

0.0065

0.213

BR-17-20

383

384

1

0.0415

0.0056

0.006

1.1

0.0005

0.046

BR-17-20

384

385

1

0.0188

0.0054

0.006

0.6

0.0002

0.137

BR-17-20

385

386

1

0.0471

0.0028

0.0002

0.441

BR-17-20

386

387

1

0.0123

0.0053

0.5

0.0001

0.046

BR-17-20

387

388

1

0.0132

0.0095

0.006

0.7

0.0002

0.046

BR-17-20

388

389

1

0.034

0.0221

0.016

1.4

0.0005

0.076

BR-17-20

389

390

1

0.0136

0.0059

0.006

0.6

0.0003

0.061

BR-17-20

390

391

1

0.0098

0.0013

0.005

0.0002

0.03

BR-17-20

391

392

1

0.499

0.535

0.02

33.6

0.184

0.669

BR-17-20

392

393

1

0.0233

0.0077

0.015

1.3

0.0005

0.076

BR-17-20

393

394

1

0.191

0.0444

0.054

9.5

0.0017

0.365

BR-17-20

394

395

1

0.0847

0.1035

0.018

7.5

0.0006

1.232

BR-17-20

395

396

1

0.223

0.0603

0.026

25.1

0.0014

0.608

BR-17-20

396

397.3

1.3

0.232

0.0769

0.024

11

0.0008

2.145

BR-17-20

397.3

398

0.7

0.123

0.0628

0.023

5.6

0.0008

0.563

BR-17-20

398

400

2

0.0989

0.0387

0.017

9

0.0033

0.593

BR-17-20

400

402

2

0.0086

0.0022

0.013

0.0004

0.046

BR-17-20

402

404

2

0.0063

0.0022

0.019

0.8

0.0004

0.061

BR-17-20

404

406

2

0.0065

0.0013

0.012

0.5

0.0006

0.046

BR-17-20

406

408

2

0.011

0.0021

0.006

0.5

0.0003

0.061

BR-17-20

408

410

2

0.0531

0.0078

0.01

0.8

0.0003

0.137

BR-17-20

410

412

2

0.0238

0.0075

0.006

0.8

0.0002

0.213

BR-17-20

412

414

2

0.0128

0.007

0.007

0.8

0.0004

0.198

BR-17-20

414

416

2

0.0149

0.007

0.5

0.0002

0.076

BR-17-20

416

417

1

0.0162

0.0037

0.006

0.6

0.0003

0.213

BR-17-20

417

417.7

0.7

0.022

0.0067

0.009

1

0.0002

0.304

BR-17-20

417.7

418.5

0.8

0.013

0.0028

0.009

0.0003

0.03

BR-17-20

418.5

420

1.5

0.008

0.0019

0.016

0.0003

0.046

BR-17-20

420

421

1

0.0106

0.0017

0.011

0.0002

0.046

BR-17-20

421

422

1

0.0072

0.0016

0.007

0.0002

0.274

BR-17-20

422

423

1

0.0254

0.0021

0.011

0.0002

0.411

BR-17-20

423

424

1

0.0191

0.0018

0.016

0.0002

0.198

BR-17-20

424

425

1

0.0458

0.0141

0.015

3

0.002

4.838

BR-17-20

425

426

1

0.0224

0.0028

0.014

0.7

0.0004

0.487

BR-17-20

426

427

1

0.0315

0.0039

0.008

0.7

0.0002

0.213

BR-17-20

427

428

1

0.0531

0.0099

0.022

6.7

0.0007

0.319

BR-17-20

428

429

1

0.0443

0.0079

0.008

0.5

0.0003

0.061

BR-17-20

429

430

1

0.0111

0.0084

0.007

0.0005

0.061

BR-17-20

430

431

1

0.017

0.0188

0.009

0.6

0.0003

0.198

BR-17-20

431

432

1

0.0456

0.0081

0.006

0.0003

0.091

BR-17-20

432

433

1

0.0288

0.0059

0.007

0.0002

0.046

BR-17-20

433

434

1

0.0705

0.0199

0.011

8.5

0.0019

0.106

BR-17-20

434

435

1

0.0316

0.0053

0.019

0.9

0.0004

0.365

BR-17-20

435

436

1

0.0277

0.0051

0.008

0.0002

0.061

BR-17-20

436

437

1

0.006

0.0049

0.009

0.0002

0.03

BR-17-20

437

438

1

0.105

0.135

0.032

6.3

0.0012

0.137

BR-17-20

438

439.4

1.4

0.0077

0.011

0.0003

0.046

BR-17-20

439.4

440

0.6

0.0123

0.0017

0.01

0.0003

0.046

BR-17-20

440

441

1

0.016

0.009

0.016

2.9

0.0005

0.091

BR-17-20

441

442

1

0.292

0.121

0.064

35.2

0.0106

2.495

BR-17-20

442

443

1

0.0306

0.0198

0.025

5.6

0.0014

0.715

BR-17-20

443

444

1

0.0044

0.0035

0.017

1.4

0.0007

0.046

BR-17-20

444

445

1

0.0067

0.0023

0.018

0.5

0.0005

0.076

BR-17-20

445

446

1

0.014

0.0087

0.026

2.1

0.0005

0.274

BR-17-20

446

447.2

1.2

0.0596

0.0264

0.034

7.8

0.0017

0.411

BR-17-20

447.2

448

0.8

0.0349

0.0136

0.02

2.8

0.0007

0.076

BR-17-20

448

449

1

0.0322

0.0582

0.017

3.6

0.0008

0.106

BR-17-20

449

450

1

0.0592

0.0725

0.022

7.9

0.0029

2.023

BR-17-20

450

451

1

0.0222

0.0112

0.016

1.4

0.0005

2.419

BR-17-20

451

452

1

0.0044

0.028

0.7

0.0004

0.821

BR-17-20

452

453

1

0.0162

0.0103

0.015

1

0.0005

0.076

BR-17-20

453

454

1

0.0124

0.0074

0.012

0.5

0.0003

0.517

BR-17-20

454

455

1

0.109

0.0188

0.011

1.3

0.0004

0.243

BR-17-20

455

456

1

0.0326

0.011

0.012

0.5

0.0002

0.046

BR-17-20

456

457

1

0.0151

0.003

0.011

0.0002

0.046

BR-17-20

457

458

1

0.0767

0.0132

0.02

1.6

0.0017

0.456

BR-17-20

458

459

1

0.0458

0.0066

0.017

1.8

0.0021

0.046

BR-17-20

459

460

1

0.0244

0.0045

0.013

0.0005

0.061

BR-17-20

460

461

1

0.0182

0.0017

0.01

0.0003

0.046

BR-17-20

461

462

1

0.0135

0.0059

0.009

1.2

0.0035

0.046

BR-17-20

462

463

1

0.0088

0.0023

0.008

0.0006

0.03

BR-17-20

463

464

1

0.011

0.0205

0.009

8.3

0.0234

0.03

BR-17-20

464

465

1

0.0122

0.0023

0.006

0.0013

0.046

BR-17-20

465

466

1

0.0144

0.0014

0.0016

0.046

BR-17-20

466

467

1

0.0111

0.0023

0.0004

0.046

BR-17-20

467

468

1

0.0099

0.0015

0.005

0.0014

0.03

BR-17-20

468

469

1

0.0084

0.001

0.011

0.0004

0.046

BR-17-20

469

470

1

0.0115

0.0011

0.018

0.007

0.061

BR-17-20

470

471

1

0.0549

0.0014

0.007

0.0012

0.259

BR-17-20

471

472

1

0.0141

0.0024

0.012

0.0035

0.03

BR-17-20

472

473

1

0.0055

0.0031

0.006

0.0023

0.061

BR-17-20

473

474

1

0.0163

0.0013

0.01

0.0104

0.046

BR-17-20

474

475

1

0.0061

0.0013

0.027

0.0013

0.061

BR-17-20

475

476

1

0.0046

0.0011

0.009

0.0024

0.03

BR-17-20

476

477

1

0.0093

0.001

0.008

0.0036

0.03

BR-17-20

477

478

1

0.0053

0.0007

0.009

0.0013

0.03

BR-17-20

478

479

1

0.0122

0.0012

0.007

0.0082

0.046

BR-17-20

479

480

1

0.0085

0.0099

0.007

0.0085

0.152

BR-17-20

480

481.2

1.2

0.0281

0.007

0.008

0.0018

1.065

BR-17-20

481.2

482.4

1.2

0.0076

0.0009

0.0004

0.046

BR-17-20

482.4

483.6

1.2

0.0077

0.0011

0.0018

0.046

BR-17-20

483.6

484.8

1.2

0.0075

0.0014

0.006

0.0018

0.091

BR-17-20

484.8

486

1.2

0.0074

0.0016

0.006

0.0006

0.046

BR-17-20

486

487.2

1.2

0.0086

0.0019

0.006

0.0027

0.046

BR-17-20

487.2

488.4

1.2

0.0119

0.0035

0.011

1.7

0.0089

0.198

BR-17-20

488.4

489.6

1.2

0.0192

0.0074

0.008

1.1

0.0185

0.046

BR-17-20

489.6

490.8

1.2

0.0209

0.0022

0.008

0.0015

0.046

BR-17-20

490.8

492

1.2

0.008

0.0011

0.0004

0.061

BR-17-20

492

493

1

0.0102

0.0038

0.007

0.0021

0.076

BR-17-20

493

494

1

0.0155

0.0026

0.005

0.0012

0.122

BR-17-20

494

495

1

0.008

0.0015

0.012

0.6

0.0055

0.106

BR-17-20

495

496

1

0.007

0.0009

0.006

0.0007

0.046

BR-17-20

496

497

1

0.0072

0.0007

0.0003

0.046

BR-17-20

497

498

1

0.0061

0.0008

0.0002

0.046

BR-17-20

498

498.5

0.5

0.0121

0.0011

0.0003

0.061

 

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-18-20

0

135

No sample

BR-18-20

135

137

2

0.01

0.001

0.0002

0.03

BR-18-20

137

139

2

0.009

0.0012

0.0006

0.106

BR-18-20

139

141

2

0.0084

0.0013

0.0002

0.03

BR-18-20

141

143

2

0.0077

0.001

0.0002

0.046

BR-18-20

143

145

2

0.0087

0.001

0.0015

0.319

BR-18-20

145

147

2

0.0082

0.0013

0.0001

0.03

BR-18-20

147

149

2

0.0074

0.0009

0.0001

0.046

BR-18-20

149

151

2

0.0073

0.0006

0.0001

0.046

BR-18-20

151

153

2

0.0102

0.0011

0.0001

0.046

BR-18-20

153

155

2

0.0093

0.0007

0.005

0.0003

0.046

BR-18-20

155

157

2

0.0128

0.0034

0.008

0.6

0.0014

0.076

BR-18-20

157

159

2

0.0075

0.001

0.0002

0.046

BR-18-20

159

161

2

0.0073

0.001

0.0001

0.046

BR-18-20

161

162

1

0.0067

0.0007

0.0001

0.061

BR-18-20

162

163

1

0.0068

0.0007

0.0002

0.152

BR-18-20

163

164

1

0.0066

0.0009

0.006

0.0001

0.061

BR-18-20

164

165

1

0.0069

0.0007

0.0001

0.35

BR-18-20

165

166

1

0.0065

0.001

0.0001

0.061

BR-18-20

166

167

1

0.0067

0.0009

0.0001

0.061

BR-18-20

167

168

1

0.0063

0.0008

0.0001

0.091

BR-18-20

168

169

1

0.0062

0.0007

0.0001

0.076

BR-18-20

169

170.15

1.15

0.006

0.0009

0.0001

0.046

BR-18-20

170.15

171

0.85

0.0055

0.0009

0.0005

0.137

BR-18-20

171

172

1

0.006

0.001

0.0004

0.183

BR-18-20

172

173.1

1.1

0.0064

0.0011

0.0073

0.639

BR-18-20

173.1

173.9

0.8

0.0039

0.0048

0.202

1

0.0066

5.994

BR-18-20

173.9

174.7

0.8

0.0292

0.0113

0.134

2.1

0.0191

2.297

BR-18-20

174.7

175.5

0.8

1.495

1.025

0.483

86.9

0.874

26.926

BR-18-20

175.5

176.5

1

1.105

0.849

0.515

69.3

1.17

38.944

BR-18-20

176.5

177.5

1

0.341

0.189

0.58

28.5

0.886

41.834

BR-18-20

177.5

178.5

1

1.365

0.749

0.845

90.8

0.847

24.644

BR-18-20

178.5

179.5

1

0.689

1.02

0.328

98

1.39

44.116

BR-18-20

179.5

180.8

1.3

2.09

1.545

0.915

136

0.568

54.308

BR-18-20

180.8

181.3

0.5

1.005

2.19

1.45

155

0.943

85.189

BR-18-20

181.3

182

0.7

1.845

2.03

1.325

167

0.548

88.688

BR-18-20

182

182.5

0.5

2.07

2.35

1.14

393

0.576

85.189

BR-18-20

182.5

183

0.5

7.7

3.93

3.61

455

0.517

74.997

BR-18-20

183

183.7

0.7

3.6

1.71

1.495

312

0.311

44.42

BR-18-20

183.7

184.5

0.8

0.13

0.367

0.035

6.4

0.036

0.837

BR-18-20

184.5

185.5

1

0.107

0.0309

0.02

6

0.0038

0.669

BR-18-20

185.5

186.5

1

0.0978

0.166

0.005

5.2

0.0083

0.487

BR-18-20

186.5

187.5

1

0.0594

0.0256

4.7

0.001

0.091

BR-18-20

187.5

188.5

1

0.0238

0.124

5.8

0.0131

0.456

BR-18-20

188.5

189.5

1

0.0105

0.0771

3.4

0.0087

1.521

BR-18-20

189.5

190.4

0.9

0.0237

0.0423

4.5

0.0148

1.582

BR-18-20

190.4

192.4

2

0.0137

0.0937

0.016

2.4

0.0133

1.384

BR-18-20

192.4

194

1.6

0.228

0.226

0.014

4.7

0.0169

0.137

BR-18-20

194

196

2

0.15

0.241

0.012

1.7

0.0132

1.536

BR-18-20

196

197.4

1.4

0.0639

0.395

0.012

3

0.0115

3.544

BR-18-20

197.4

198.4

1

0.0057

0.0065

0.0023

0.061

BR-18-20

198.4

199.4

1

0.0036

0.0016

0.001

0.03

BR-18-20

199.4

200.4

1

0.0049

0.0021

0.0028

0.046

BR-18-20

200.4

201

0.6

0.0066

0.0011

0.9

0.0126

0.046

BR-18-20

201

201.3

0.3

No sample

BR-18-20

201.3

202.3

1

0.0051

0.0028

0.0017

0.106

BR-18-20

202.3

202.8

0.5

No sample

BR-18-20

202.8

204.8

2

0.0069

0.002

0.0011

0.015

BR-18-20

204.8

206.8

2

0.0066

0.002

0.0011

0.03

BR-18-20

206.8

208.8

2

0.0067

0.0103

0.0026

0.03

BR-18-20

208.8

210.8

2

0.0089

0.004

0.0022

0.061

BR-18-20

210.8

212.8

2

0.0112

0.0111

0.037

0.0104

0.03

BR-18-20

212.8

214.8

2

0.015

0.137

0.048

1.3

0.0316

0.167

BR-18-20

214.8

216.8

2

0.0067

0.0034

0.0018

0.198

BR-18-20

216.8

218.8

2

0.0064

0.003

0.0015

0.03

BR-18-20

218.8

220.8

2

0.0102

0.0058

0.0042

0.03

BR-18-20

220.8

222.8

2

0.008

0.0152

0.007

0.0034

1.445

BR-18-20

222.8

224.2

1.4

0.0088

0.0048

0.009

0.0031

0.03

BR-18-20

224.2

225

0.8

0.07

0.0568

0.026

1.2

0.0153

0.015

BR-18-20

225

226

1

0.0558

0.105

0.032

1.6

0.0186

0.122

BR-18-20

226

227

1

0.134

0.108

0.012

5.6

0.0088

0.532

BR-18-20

227

228

1

0.0604

0.152

0.04

1.6

0.0252

3.544

BR-18-20

228

229

1

0.0781

0.13

0.037

1.2

0.0167

1.749

BR-18-20

229

231

2

0.197

0.426

0.253

2.4

0.0157

9.493

BR-18-20

231

233

2

0.675

1.015

0.261

10.3

0.0441

0.365

BR-18-20

233

235

2

0.54

0.249

0.07

113

0.05

0.426

BR-18-20

235

237

2

0.239

0.115

0.059

45.4

0.0097

0.183

BR-18-20

237

239

2

0.876

0.28

0.145

69.4

0.0376

0.837

BR-18-20

239

241

2

0.259

0.128

0.053

16

0.0172

0.183

BR-18-20

241

243

2

0.328

0.176

0.044

38.1

0.0334

0.867

BR-18-20

243

245

2

0.0697

0.187

0.079

48.8

0.0304

0.487

BR-18-20

245

247

2

0.267

0.346

0.132

86

0.0303

1.749

BR-18-20

247

249

2

0.155

0.364

0.106

162

0.0408

1.278

BR-18-20

249

251

2

0.212

0.194

0.057

81.3

0.0202

0.426

BR-18-20

251

253

2

0.327

0.112

0.039

51.4

0.0086

0.821

BR-18-20

253

255

2

0.335

0.0954

0.042

47.5

0.0108

0.426

BR-18-20

255

257

2

0.325

0.0831

0.019

39.4

0.011

0.821

BR-18-20

257

259

2

0.113

0.0544

0.013

25

0.022

0.106

BR-18-20

259

261

2

0.2

0.132

0.052

38.4

0.0327

0.243

BR-18-20

261

263

2

0.123

0.0807

0.083

16.9

0.0162

0.304

BR-18-20

263

265

2

0.237

0.0733

0.056

96.6

0.0296

0.396

BR-18-20

265

267

2

0.451

0.113

0.024

116

0.0433

0.228

BR-18-20

267

269

2

0.156

0.0504

0.024

28.2

0.0097

0.167

BR-18-20

269

271

2

0.0898

0.0391

0.013

4.8

0.0046

0.38

BR-18-20

271

272.5

1.5

0.0655

0.0184

2.9

0.0015

0.426

BR-18-20

272.5

273.1

0.6

0.0568

0.0203

4.1

0.0027

0.213

BR-18-20

273.1

275

1.9

0.0182

0.0048

0.005

2.6

0.0016

0.213

BR-18-20

275

277

2

0.0625

0.0164

3.3

0.0018

0.365

BR-18-20

277

279

2

0.0837

0.021

6

0.0028

0.183

BR-18-20

279

281

2

0.0317

0.0076

4.4

0.0019

0.137

BR-18-20

281

283

2

0.0257

0.0061

2.8

0.0013

0.137

BR-18-20

283

285

2

0.0394

0.0063

5.2

0.0015

0.335

BR-18-20

285

287

2

0.0244

0.0069

4.5

0.0016

0.183

BR-18-20

287

289

2

0.0339

0.0047

3.4

0.0017

0.152

BR-18-20

289

291

2

0.0171

0.0041

3.8

0.0012

0.517

BR-18-20

291

293

2

0.0143

0.0036

4

0.0013

0.137

BR-18-20

293

294.5

1.5

0.023

0.0103

2.7

0.0023

0.411

BR-18-20

294.5

296.5

2

0.0335

0.0216

2.5

0.198

BR-18-20

296.5

297.1

0.6

0.0345

0.016

1

0.003

0.046

BR-18-20

297.1

299

1.9

0.0397

0.012

0.0027

0.122

BR-18-20

299

301

2

0.0152

0.005

1.9

0.0022

0.198

BR-18-20

301

303

2

0.0491

0.021

4.7

0.0026

0.396

BR-18-20

303

305

2

0.0224

0.0115

0.006

11.6

0.003

0.319

BR-18-20

305

307

2

0.0145

0.0143

12.2

0.0021

0.35

BR-18-20

307

309

2

0.0279

0.0146

7.8

0.0019

0.35

BR-18-20

309

311

2

0.0116

0.007

9.9

0.0022

0.243

BR-18-20

311

313

2

0.042

0.0122

6.5

0.0014

0.335

BR-18-20

313

315

2

0.0584

0.0284

24

0.0051

1.019

BR-18-20

315

317

2

0.016

0.0061

11.9

0.0031

0.487

BR-18-20

317

319

2

0.0133

0.007

0.005

6.8

0.0018

0.502

BR-18-20

319

321

2

0.0334

0.0129

4.5

0.003

0.487

BR-18-20

321

323

2

0.0151

0.0039

1.4

0.0016

0.198

BR-18-20

323

325

2

0.0324

0.0073

2.4

0.0021

0.487

BR-18-20

325

327

2

0.0155

0.0047

1.8

0.0018

0.304

BR-18-20

327

329

2

0.0204

0.0085

2.4

0.0029

0.365

BR-18-20

329

331

2

0.0271

0.0078

1.9

0.335

BR-18-20

331

333

2

0.0338

0.0077

2.4

0.0018

0.472

BR-18-20

333

335

2

0.0337

0.0117

2

0.0015

0.441

BR-18-20

335

337

2

0.0239

0.0725

0.005

4.9

0.003

0.989

BR-18-20

337

338

1

0.0243

0.0607

0.009

14.6

0.0069

0.958

BR-18-20

338

339

1

0.161

0.0736

0.011

13.1

0.0023

1.491

BR-18-20

339

340

1

0.291

0.142

0.057

39.8

0.0059

4.168

BR-18-20

340

341

1

0.257

0.107

0.025

18.8

0.0028

1.582

BR-18-20

341

342.4

1.4

0.176

0.109

0.008

36.4

0.0067

0.776

BR-18-20

342.4

344

1.6

0.0467

0.01

0.005

7.9

0.0029

0.274

BR-18-20

344

346

2

0.0094

0.0029

1.5

0.0024

0.183

BR-18-20

346

348

2

0.0121

0.0007

0.0003

0.076

BR-18-20

348

350

2

0.0108

0.0016

0.0038

0.091

BR-18-20

350

352

2

0.0083

0.0012

0.0018

0.228

BR-18-20

352

354

2

0.0081

0.0014

0.0036

0.076

BR-18-20

354

356

2

0.0071

0.0008

0.001

0.076

BR-18-20

356

357

1

0.0069

0.001

0.0028

0.091

BR-18-20

357

358.8

1.8

0.0074

0.0008

0.0005

0.137

BR-18-20

358.8

360

1.2

0.0071

0.0008

0.0013

0.076

BR-18-20

360

361

1

0.0077

0.0008

0.007

0.0035

0.046

BR-18-20

361

362.2

1.2

0.0073

0.0009

0.0018

0.091

BR-18-20

362.2

364

1.8

0.0073

0.0009

0.001

0.076

BR-18-20

364

366

2

0.0062

0.0008

0.0024

0.061

BR-18-20

366

368

2

0.0057

0.0006

0.001

0.076

BR-18-20

368

370

2

0.0054

0.0006

0.0016

0.061

BR-18-20

370

372

2

0.0068

0.0005

0.0065

0.106

BR-18-20

372

374

2

0.0071

0.0005

0.0022

0.122

BR-18-20

374

376

2

0.0052

0.0006

0.0012

0.106

BR-18-20

376

378

2

0.0058

0.0007

0.007

0.0005

0.091

BR-18-20

378

380

2

0.0058

0.0008

0.006

0.0011

0.091

BR-18-20

380

380.9

0.9

0.0046

0.0005

0.007

0.0031

0.03

BR-18-20

380.9

382.4

1.5

0.0065

0.0008

0.008

0.0013

0.076

BR-18-20

382.4

384

1.6

0.0048

0.0004

0.009

0.0018

0.183

BR-18-20

384

386

2

0.005

0.0003

0.0006

0.076

BR-18-20

386

388

2

0.0072

0.0011

0.009

0.0034

0.061

BR-18-20

388

390

2

0.006

0.0012

0.014

0.0006

0.046

BR-18-20

390

392

2

0.0055

0.0009

0.009

0.0019

0.046

BR-18-20

392

394

2

0.0046

0.0006

0.02

0.0023

0.046

BR-18-20

394

396

2

0.0064

0.0006

0.022

0.0016

0.046

BR-18-20

396

398

2

0.0067

0.0007

0.009

0.0011

0.046

BR-18-20

398

400

2

0.0056

0.0006

0.015

0.0005

0.046

BR-18-20

400

402

2

0.0057

0.0003

0.009

0.0012

0.03

BR-18-20

402

404

2

0.0062

0.0003

0.008

0.0006

0.046

BR-18-20

404

406

2

0.0061

0.0005

0.008

0.0006

0.091

BR-18-20

406

408

2

0.0081

0.0005

0.009

0.002

0.03

BR-18-20

408

410

2

0.0072

0.0006

0.006

0.0021

0.091

BR-18-20

410

412

2

0.0079

0.0006

0.005

0.002

0.076

BR-18-20

412

414

2

0.007

0.001

0.005

0.0021

0.046

BR-18-20

414

416

2

0.011

0.0017

0.043

0.0041

0.152

BR-18-20

416

418

2

0.0084

0.0017

0.018

0.0026

0.319

BR-18-20

418

420

2

0.0102

0.0021

0.009

0.0019

0.137

BR-18-20

420

422

2

0.0168

0.0019

0.015

0.0011

0.046

BR-18-20

422

432

10

No sample

BR-18-20

432

434

2

0.0091

0.0009

0.008

0.001

0.03

BR-18-20

434

435

1

0.0268

0.0012

0.005

0.0006

0.122

BR-18-20

435

436.3

1.3

0.0307

0.0017

0.007

0.0008

0.578

BR-18-20

436.3

437

0.7

0.0085

0.0076

0.046

0.002

0.106

BR-18-20

437

438.3

1.3

0.0141

0.0033

0.022

0.0006

0.091

BR-18-20

438.3

440

1.7

0.0113

0.0028

0.011

0.0012

0.046

BR-18-20

440

442

2

0.0161

0.0018

0.005

0.0009

0.228

BR-18-20

442

444

2

0.0119

0.0017

0.011

0.0013

0.091

BR-18-20

444

446

2

0.0104

0.0018

0.005

0.0011

0.091

BR-18-20

446

448

2

0.0121

0.0045

0.0014

0.076

BR-18-20

448

450

2

0.0121

0.0106

0.022

0.5

0.0017

0.106

BR-18-20

450

451

1

0.0171

0.0042

0.014

0.0008

0.502

BR-18-20

451

452.6

1.6

0.215

0.0088

0.017

0.8

0.0066

0.167

BR-18-20

452.6

454

1.4

0.0165

0.0078

0.01

0.5

0.0203

0.441

BR-18-20

454

456

2

0.0089

0.0027

0.009

0.004

0.122

BR-18-20

456

457

1

0.0088

0.0008

0.0002

0.122

BR-18-20

457

458.4

1.4

0.0101

0.0008

0.0078

0.198

BR-18-20

458.4

460

1.6

0.0086

0.0009

0.008

0.0002

0.076

BR-18-20

460

461

1

0.0094

0.0006

0.007

0.0001

0.152

BR-18-20

461

462.3

1.3

0.0094

0.0011

0.0001

0.122

BR-18-20

462.3

464

1.7

0.0108

0.0012

0.0012

0.152

BR-18-20

464

466

2

0.0083

0.0036

0.009

0.002

0.091

BR-18-20

466

468

2

0.0088

0.0027

0.0018

0.076

BR-18-20

468

469

1

0.0182

0.0045

0.042

0.5

0.0021

0.152

BR-18-20

469

470.2

1.2

0.0317

0.0033

0.019

0.0015

0.213

BR-18-20

470.2

471.4

1.2

No sample

BR-18-20

471.4

472.5

1.1

0.0085

0.0005

0.0002

0.046

BR-18-20

472.5

474.5

2

0.0111

0.0008

0.0002

0.091

BR-18-20

474.5

476.5

2

0.0101

0.001

0.0003

0.106

BR-18-20

476.5

478.5

2

0.009

0.0011

0.0018

0.183

BR-18-20

478.5

480.5

2

0.0107

0.0015

0.007

0.0008

0.152

BR-18-20

480.5

482.5

2

0.0101

0.0021

0.009

0.0015

0.411

BR-18-20

482.5

484.5

2

0.0296

0.0163

0.01

1.2

0.0044

0.122

BR-18-20

484.5

485.1

0.6

0.013

0.0029

0.0037

0.046

BR-18-20

485.1

486.5

1.4

0.0108

0.0037

0.0032

0.061

BR-18-20

486.5

488.5

2

0.0135

0.001

0.0013

0.046

BR-18-20

488.5

490.5

2

0.0121

0.0057

0.005

0.0227

0.213

BR-18-20

490.5

492.5

2

0.0103

0.0053

0.005

0.0011

0.122

BR-18-20

492.5

494.5

2

0.0112

0.0059

0.0046

0.091

BR-18-20

494.5

496.5

2

0.0103

0.0008

0.0012

0.061

BR-18-20

496.5

498.5

2

0.0124

0.0005

0.0007

0.076

BR-18-20

498.5

500

1.5

0.0136

0.0049

0.006

0.0081

0.061

BR-18-20

500

501

1

0.0138

0.0019

0.0114

0.106

BR-18-20

501

502.1

1.1

0.0093

0.0035

1

0.163

0.061

BR-18-20

502.1

504

1.9

0.0106

0.0013

0.066

0.076

BR-18-20

504

506

2

0.0116

0.0009

0.0119

0.152

BR-18-20

506

508

2

0.0124

0.0012

0.007

0.0005

0.076

BR-18-20

508

510

2

0.0214

0.0144

0.005

0.028

0.152

BR-18-20

510

512

2

0.0205

0.0154

0.007

0.7

0.0093

0.426

BR-18-20

512

513.4

1.4

0.0114

0.0028

0.01

0.0112

0.106

BR-18-20

513.4

514.1

0.7

0.0119

0.0008

0.013

0.0004

0.228

BR-18-20

514.1

515.7

1.6

0.0133

0.0013

0.006

0.0014

0.122

BR-18-20

515.7

517

1.3

0.0093

0.0009

0.0002

0.061

BR-18-20

517

519

2

0.0091

0.0005

0.007

0.0003

0.076

BR-18-20

519

521

2

0.0081

0.0007

0.006

0.0001

0.076

BR-18-20

521

522.6

1.6

0.0081

0.0005

0.0001

0.152

BR-18-20

522.6

524

1.4

0.0049

0.0012

0.006

0.0004

0.137

BR-18-20

524

526

2

0.0122

0.0011

0.019

0.002

0.106

BR-18-20

526

528

2

0.0132

0.0034

0.0018

0.061

BR-18-20

528

530

2

0.0136

0.0057

0.033

0.0372

0.076

BR-18-20

530

532

2

0.0133

0.0028

0.009

0.0021

0.167

BR-18-20

532

534

2

0.0112

0.0015

0.006

0.0013

0.076

BR-18-20

534

536

2

0.0107

0.0012

0.0014

0.046

BR-18-20

536

537.7

1.7

0.0131

0.0022

0.007

0.0023

0.274

BR-18-20

537.7

539

1.3

0.0079

0.0241

0.012

0.8

0.005

0.106

BR-18-20

539

541

2

0.0049

0.0026

0.011

0.0004

0.061

BR-18-20

541

543

2

0.0079

0.0007

0.0002

0.061

BR-18-20

543

545

2

0.0099

0.0009

0.0002

0.061

BR-18-20

545

547

2

0.0051

0.0006

0.0001

0.046

BR-18-20

547

549

2

0.0059

0.0007

0.0001

0.046

BR-18-20

549

551

2

0.004

0.0007

0.007

0.0005

0.046

BR-18-20

551

553

2

0.0049

0.0018

0.0002

0.152

BR-18-20

553

555

2

0.0055

0.0008

0.0016

0.061

BR-18-20

555

557

2

0.005

0.001

0.0122

0.046

BR-18-20

557

558

1

0.0067

0.0018

0.0001

0.091

BR-18-20

558

560

2

0.0081

0.001

0.006

0.0001

0.046

BR-18-20

560

562

2

0.0056

0.0026

0.014

0.0019

0.076

BR-18-20

562

564

2

0.0843

0.0281

0.144

1

0.0142

0.259

BR-18-20

564

566

2

0.0035

0.0012

0.019

0.0004

0.076

BR-18-20

566

568

2

0.0045

0.0014

0.007

0.0012

0.122

BR-18-20

568

570

2

0.004

0.0011

0.005

0.0003

0.091

BR-18-20

570

572

2

0.004

0.0007

0.0001

0.061

BR-18-20

572

574

2

0.0062

0.0106

1.6

0.0202

0.137

BR-18-20

574

576

2

0.0026

0.0031

0.017

0.6

0.0044

0.304

BR-18-20

576

578

2

0.0029

0.006

0.008

0.7

0.0091

0.122

BR-18-20

578

580

2

0.0114

0.0206

0.005

1.5

0.054

0.563

BR-18-20

580

582

2

0.0036

0.0023

0.006

0.0009

0.137

BR-18-20

582

584

2

0.0059

0.0013

0.005

0.0002

0.091

BR-18-20

584

586

2

0.005

0.001

0.0001

0.061

BR-18-20

586

587

1

0.0039

0.0009

0.007

0.0001

0.076

BR-18-20

587

588.3

1.3

0.0036

0.0016

0.022

0.0002

0.076

BR-18-20

588.3

590

1.7

0.0058

0.0023

0.0001

0.167

BR-18-20

590

592

2

0.0057

0.0008

0.011

0.0001

0.228

BR-18-20

592

594

2

0.0062

0.0008

0.008

0.0001

0.076

BR-18-20

594

596

2

0.0047

0.0008

0.005

0.0001

0.076

BR-18-20

596

598

2

0.0034

0.0007

0.0001

0.091

BR-18-20

598

600

2

0.0056

0.0022

0.006

0.0001

0.228

BR-18-20

600

602

2

0.0093

0.0016

0.026

0.0001

0.228

BR-18-20

602

604

2

0.0055

0.0009

0.106

BR-18-20

604

606

2

0.0063

0.0028

0.0001

0.076

BR-18-20

606

607

1

0.0073

0.0019

0.014

0.0001

0.122

 

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-20-20

225

227

2

0.0094

0.0049

0.054

2.9

0.0033

0.122

BR-20-20

227

228.2

1.2

0.0346

0.0852

0.024

7.1

0.0201

1.871

BR-20-20

228.2

229

0.8

1.56

1.58

0.537

112

0.291

53.091

BR-20-20

229

230

1

0.116

1.01

0.6

75.9

0.157

54.004

BR-20-20

230

231

1

0.739

1.55

0.618

85.2

0.424

38.335

BR-20-20

231

232

1

1.305

0.851

0.5

141

0.612

11.577

BR-20-20

232

233.2

1.2

1.105

0.423

0.4

46

0.0431

4.853

BR-20-20

233.2

234

0.8

1.505

2.64

0.666

164

0.796

31.185

BR-20-20

234

235

1

3.35

2.74

0.858

229

0.993

28.295

BR-20-20

235

235.5

0.5

2.64

2.33

0.719

226

0.931

30.197

BR-20-20

235.5

237

1.5

1.4

0.929

0.327

50.2

0.185

8.291

BR-20-20

237

238

1

3.14

2.07

0.502

40.7

0.562

1.323

BR-20-20

238

239

1

0.259

0.181

0.109

7.6

0.0662

2.647

BR-20-20

239

240

1

0.488

0.366

0.15

8.1

0.0676

0.761

BR-20-20

240

241

1

0.395

0.303

0.111

7.9

0.154

0.046

BR-20-20

241

241.5

0.5

0.207

0.0326

0.076

2

0.0117

1.552

BR-20-20

241.5

243

1.5

0.0125

0.0073

0.007

0.004

0.882

BR-20-20

243

245

2

0.0109

0.0051

0.009

0.0034

0.213

BR-20-20

245

247

2

0.0114

0.0127

0.007

0.0037

0.122

BR-20-20

247

248.7

1.7

0.0097

0.0089

0.011

0.0033

0.061

BR-20-20

248.7

250.2

1.5

0.0159

0.0015

0.0028

0.03

BR-20-20

250.2

252.2

2

0.0245

0.0018

0.0086

0.015

 

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-22-20

0

184

No sample

BR-22-20

184

186

2

0.0409

0.0069

0.039

0.9

0.03

0.426

BR-22-20

186

188

2

0.0227

0.0035

0.018

0.0011

0.517

BR-22-20

188

190

2

0.41

0.1795

0.109

4.8

0.001

3.21

BR-22-20

190

192

2

0.031

0.002

0.016

0.0012

0.152

BR-22-20

192

194

2

0.0232

0.0008

0.011

0.001

0.03

BR-22-20

194

196

2

0.0103

0.0016

0.01

0.0006

0.046

BR-22-20

196

198

2

0.0179

0.0008

0.017

0.0006

0.008

BR-22-20

198

200

2

0.004

0.0053

0.02

0.0009

0.046

BR-22-20

200

202

2

0.0092

0.0017

0.018

0.0007

0.015

BR-22-20

202

204

2

0.0097

0.0032

0.038

0.0015

0.015

BR-22-20

204

206

2

0.0102

0.0045

0.101

0.015

BR-22-20

206

208

2

0.0197

0.0031

0.09

0.0013

0.03

BR-22-20

208

210

2

0.0085

0.0058

0.12

0.0022

0.183

BR-22-20

210

212

2

0.0072

0.0211

0.176

0.7

0.0091

0.624

BR-22-20

212

214

2

0.0139

0.0082

0.113

0.6

0.0019

0.106

BR-22-20

214

216

2

0.143

0.246

0.329

2.1

0.0418

1.263

BR-22-20

216

218

2

0.0387

0.0358

0.4

2.1

0.133

0.046

BR-22-20

218

219.7

1.7

0.177

0.0265

0.256

1.5

0.0204

0.106

BR-22-20

219.7

220.7

1

0.169

0.291

0.905

8.6

0.472

0.046

BR-22-20

220.7

221.7

1

0.0183

0.009

0.178

1.3

0.0041

0.015

BR-22-20

221.7

222.7

1

0.0176

0.0111

0.143

0.8

0.0037

0.03

BR-22-20

222.7

223.7

1

0.0787

0.307

0.575

5.1

0.16

0.228

BR-22-20

223.7

224.7

1

0.104

0.1335

0.481

3.8

0.0502

1.187

BR-22-20

224.7

225.7

1

0.236

0.1465

0.921

7.8

0.117

1.719

BR-22-20

225.7

226.3

0.6

0.221

0.182

1.185

7.9

0.0752

0.7

BR-22-20

226.3

227

0.7

0.135

0.975

1.865

11.4

0.326

4.549

BR-22-20

227

228

1

0.211

0.0523

0.482

6.2

0.0829

6.648

BR-22-20

228

229

1

0.39

0.1055

0.652

16

0.281

4.853

BR-22-20

229

230

1

0.0372

0.0082

0.153

0.7

0.0108

0.122

BR-22-20

230

231

1

0.0518

0.0081

0.152

1

0.0092

0.624

BR-22-20

231

232

1

0.663

0.073

1.05

11.8

0.144

9.432

BR-22-20

232

233

1

0.209

0.0739

0.553

9

0.0355

3.453

BR-22-20

233

234

1

0.246

0.119

0.489

16.4

0.015

2.16

BR-22-20

234

235

1

0.0222

0.0223

0.502

5.1

0.0093

0.837

BR-22-20

235

236

1

0.0232

0.0127

0.555

2

0.0081

0.806

BR-22-20

236

237

1

0.0256

0.026

0.152

1.4

0.0051

0.061

BR-22-20

237

237.7

0.7

0.0294

0.051

0.383

3.7

0.0507

0.35

BR-22-20

237.7

238.2

0.5

0.281

0.169

1.83

33.3

2.19

1.78

BR-22-20

238.2

239.2

1

0.0196

0.0689

0.173

1.8

0.0493

0.685

BR-22-20

239.2

240.4

1.2

0.0983

0.131

0.927

7.6

0.122

2.464

BR-22-20

240.4

241.2

0.8

0.087

0.079

2.3

23.7

0.418

2.038

BR-22-20

241.2

242.1

0.9

0.0946

0.0209

0.414

3.8

0.175

5.218

BR-22-20

242.1

243.2

1.1

0.0034

0.0159

0.318

1.4

0.0057

1.917

BR-22-20

243.2

244.1

0.9

0.151

0.037

1.075

13.2

1.265

0.259

BR-22-20

244.1

245

0.9

0.141

0.0044

0.13

0.0379

0.913

BR-22-20

245

246

1

0.231

0.0067

0.166

0.9

0.0107

2.951

BR-22-20

246

247

1

0.0472

0.0074

0.132

0.5

0.0038

0.898

BR-22-20

247

248

1

0.0043

0.0043

0.044

0.0012

0.015

BR-22-20

248

249

1

0.0043

0.0087

0.203

0.6

0.0042

0.243

BR-22-20

249

250

1

0.0353

0.0115

0.189

0.0101

0.137

BR-22-20

250

251

1

0.111

0.0125

0.237

1

0.0071

0.35

BR-22-20

251

252

1

0.0209

0.0055

0.107

0.0014

0.167

BR-22-20

252

253

1

0.193

0.009

0.334

2

0.0116

4.944

BR-22-20

253

254

1

0.13

0.0073

0.337

1.1

0.0042

10.497

BR-22-20

254

255.2

1.2

0.12

0.0125

0.488

1.6

0.0153

5.431

BR-22-20

255.2

256

0.8

0.213

0.0086

0.178

0.0031

0.091

BR-22-20

256

257

1

0.21

0.0156

0.345

0.0044

0.396

BR-22-20

257

258

1

0.216

0.0056

0.138

0.0029

0.243

BR-22-20

258

259

1

0.651

0.0522

0.279

2.5

0.0286

0.061

BR-22-20

259

260

1

0.928

0.439

2.42

17.9

0.1115

0.958

BR-22-20

260

261

1

1.675

0.405

1.45

39.3

0.352

0.213

BR-22-20

261

262

1

0.606

0.201

0.395

11

0.047

1.141

BR-22-20

262

263

1

0.213

0.0807

0.32

3.6

0.0269

0.106

BR-22-20

263

264

1

0.34

0.132

0.751

5.1

0.0511

0.806

BR-22-20

264

265

1

0.0803

0.0116

0.537

2.6

0.249

0.578

BR-22-20

265

266

1

0.0218

0.0104

0.344

0.9

0.0047

0.259

BR-22-20

266

267

1

0.0746

0.0409

0.365

2.9

0.0275

0.7

BR-22-20

267

268

1

0.0517

0.0042

0.174

0.0024

0.061

BR-22-20

268

269

1

0.022

0.0064

0.144

0.0022

0.259

BR-22-20

269

270

1

0.109

0.0062

0.235

1.8

0.0034

0.274

BR-22-20

270

271

1

0.038

0.0045

0.153

1

0.0021

0.122

BR-22-20

271

272

1

0.137

0.0528

0.776

9.9

0.183

0.259

BR-22-20

272

273

1

0.0876

0.0763

0.626

5.9

0.073

0.106

BR-22-20

273

274

1

0.0695

0.0559

0.877

6.1

0.0096

0.152

BR-22-20

274

275

1

0.435

0.0184

0.619

4.3

0.0089

0.608

BR-22-20

275

276

1

0.596

0.0352

1.075

8.6

0.0222

0.289

BR-22-20

276

277

1

0.0539

0.0059

0.173

0.8

0.0044

0.243

BR-22-20

277

278

1

0.0724

0.0117

0.201

1.5

0.0086

0.319

BR-22-20

278

278.3

0.3

0.0113

0.0126

0.45

3.1

0.0074

0.958

BR-22-20

278.3

280

1.7

0.0168

0.0077

0.132

4.2

0.0026

0.152

BR-22-20

280

282

2

0.0135

0.0089

0.065

1.8

0.0024

0.122

BR-22-20

282

284

2

0.394

0.102

0.06

5.2

0.024

0.335

BR-22-20

284

286

2

0.237

0.0667

0.084

3.3

0.0073

1.232

BR-22-20

286

288

2

0.138

0.0371

0.04

2.1

0.0053

0.624

BR-22-20

288

290

2

0.0785

0.0155

0.032

0.7

0.0014

0.106

BR-22-20

290

292

2

0.208

0.0161

0.027

1.2

0.0047

0.715

BR-22-20

292

294

2

0.184

0.007

0.025

0.6

0.001

0.578

BR-22-20

294

295.6

1.6

0.0341

0.0031

0.023

0.5

0.0011

0.076

BR-22-20

295.6

297

1.4

0.0473

0.0115

0.022

0.0022

0.076

BR-22-20

297

299

2

0.0093

0.005

0.03

0.5

0.0011

0.046

BR-22-20

299

301

2

0.0848

0.0092

0.025

0.0008

0.046

BR-22-20

301

303

2

0.0683

0.0834

0.015

1

0.0006

0.076

BR-22-20

303

305

2

0.0654

0.0041

0.029

0.9

0.0009

0.091

BR-22-20

305

307

2

0.253

0.0385

0.033

6.9

0.0036

0.472

BR-22-20

307

309

2

1.57

0.392

0.041

30.7

0.0208

3.195

BR-22-20

309

311

2

0.996

0.238

0.036

24.5

0.0087

4.123

BR-22-20

311

312.7

1.7

0.592

0.0896

0.041

16.5

0.0097

2.495

 

 

Hole ID

From

To

Interval

Zn %

Pb %

Au g/t

Ag g/t

Cu %

BaSO4

BR-23-20

0

320

No sample

BR-23-20

320

322

2

0.0139

0.0024

0.01

0.0038

0.243

BR-23-20

322

324

2

0.012

0.0029

0.005

0.0007

0.548

BR-23-20

324

325.7

1.7

0.0182

0.578

0.381

6.9

0.0109

51.418

BR-23-20

325.7

326.4

0.7

0.0233

0.586

0.363

11.1

0.0109

90.057

BR-23-20

326.4

327

0.6

0.11

0.0411

0.353

3.1

0.0035

80.474

BR-23-20

327

328

1

0.0063

0.401

0.348

5.6

0.0052

80.93

BR-23-20

328

329

1

0.0209

0.844

2.5

123

0.0942

75.149

BR-23-20

329

330

1

4.33

12.9

1.105

963

0.973

68.152

BR-23-20

330

331

1

0.622

8.26

2.04

741

0.872

80.017

BR-23-20

331

332

1

3.49

5.12

2.48

829

1.045

76.823

BR-23-20

332

333

1

10.9

7.05

1.09

325

0.641

66.782

BR-23-20

333

334

1

10.2

4.08

1.075

211

0.389

59.328

BR-23-20

334

335

1

8.15

3.65

0.891

268

0.314

58.568

BR-23-20

335

336

1

5.26

2.17

0.95

242

0.443

49.897

BR-23-20

336

337

1

2.2

1.15

1.09

196

0.319

42.747

BR-23-20

337

338

1

1.86

2.97

0.899

200

0.498

38.335

BR-23-20

338

338.6

0.6

1.88

1.55

1.035

274

0.409

11.257

BR-23-20

338.6

339.1

0.5

0.586

0.603

0.591

40.9

0.423

11.181

BR-23-20

339.1

340

0.9

0.365

0.107

0.516

26.9

1.06

47.158

BR-23-20

340

340.7

0.7

0.0495

0.11

0.15

4.4

0.111

2.693

BR-23-20

340.7

341.3

0.6

0.031

0.019

0.096

10.9

0.14

11.729

BR-23-20

341.3

342.6

1.3

0.992

0.804

0.421

49.7

0.273

7.028

BR-23-20

342.6

344

1.4

0.0234

0.0288

0.054

1

0.0033

3.879

BR-23-20

344

346

2

0.0216

0.006

0.008

0.0081

0.289

BR-23-20

346

368

22

No sample

 APPENDIX 1: RUPICE MRE JORC TABLES

Section 1 Sampling Techniques and Data

(Criteria in this section apply to all succeeding sections.)

 

Criteria

JORC Code Explanation

Commentary

Sampling techniques

Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling.

PQ3 and HQ3 diamond core was cut in half to provide a sample for assay typically weighing around 4-6kg. Samples were submitted to the ALS facility in Bor, Serbia for industry standard analytical analysis.

 

Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.

The half core and weight of the sample is sufficiently representative.

 

No calibration of any equipment was required as all samples were sent for assay by a commercial laboratory.

Aspects of the determination of mineralisation that are Material to the Public Report. In cases where 'industry standard' work has been done this would be relatively simple (e.g. 'reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay'). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information.

PQ3 and HQ3 diamond core was used to obtain nominally 1m samples from which 4-6kg of material was pulverised to produce sample for fire assay, ICP-MS and X-ray Fluorescence (XRF).

Drilling techniques

Drill type (e.g. core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (e.g. core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc).

 

 

 

 

 

 

 

 

 

Drill sample recovery

Method of recording and assessing core and chip sample recoveries and results assessed.

All core was logged for geology and RQD with recovery in the mineralised and sampled zone greater than 90%. The PQ3 and HQ3 diameter and sampling of half core ensured the representative nature of the samples.

There is no observed relationship between sample recovery and grade, and with little to no loss of material there is considered to be little to no sample bias.

Measures taken to maximise sample recovery and ensure representative nature of the samples.

Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.

Logging

Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.

Diamond drill core samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. Not all drill holes penetrated the massive sulphide mineralisation, but all were used to guide the geological interpretations supporting the Mineral Resource estimates.

Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography.

 

All core is photographed, and logging is qualitative.

The total length and percentage of the relevant intersections logged.

All core is logged.

Sub-sampling techniques and sample preparation

If core, whether cut or sawn and whether quarter, half or all core taken.

The diamond core was cut in half using a diamond saw. Nominally 1 in 30 samples was cut in quarters, and both halves analysed (for purposes of field duplicates).

If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry.

Not applicable, as all samples are core.

For all sample types, the nature, quality and appropriateness of the sample preparation technique.

Collection of around 4-6kg of half core material with subsequent pulverisation of the total charge provided an appropriate and representative sample for analysis. Sample preparation was undertaken at the ALS laboratory in Bor, to industry best practice.

Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples.

Whole rock blanks and certified standards (~1 in 15) were introduced to the sample run to ensure laboratory QAQC. Additionally, industry best practice was adopted by ALS for laboratory sub-sampling and the avoidance of any cross contamination.

Measures taken to ensure that the sampling is representative of the in-situ material collected, including for instance results for field duplicate/second-half sampling.

The half core sampling is considered a reasonable representation of the in-situ material. Nominally 1 in 30 samples were cut in quarters, and both halves analyses (for purposes of field duplicates).

Whether sample sizes are appropriate to the grain size of the material being sampled.

Sample size of around 4-6kg is considered to be appropriate to reasonably represent the material being tested.

Quality of assay data and laboratory tests

The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total.

Analyses were undertaken at the accredited laboratory of ALS in Bor, Serbia which has full industry certification. Multi elements were assayed by an ICP-AES technique following a four-acid digest. Gold was determined using a fire assay on a nominal 50g charge. Barite was determined from a lithium borate fusion followed by dissolution and ICP-AES analysis. Total sulphur was determined by Leco.

All techniques were appropriate for the elements being determined. Samples are considered a partial digestion when using an aqua regia digest.

For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.

There was no reliance on determination of analysis by geophysical tools.

Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.

Certified Reference Material ("CRM") appropriate for the elements being analysed were added at a rate better than 1 in 15. All results reported by ALS on the CRMs were better than 2 standard deviations (2SD), it is considered that acceptable levels of accuracy have been achieved.

Additional lab checks were sent to SGS in Bor. To date,154 samples were submitted for check assaying from within the mineralised drill intercepts. The check assays correlated within tolerance to the original ALS assays.

Verification of sampling and assaying

The verification of significant intersections by either independent or alternative company personnel.

There has been no independent logging of mineralised intervals, however, it has been logged by several company personnel and verified by senior staff.

The use of twinned holes.

None of the reported holes are twin holes.

Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.

Data is stored on the Virtual Cloud and at various locations including Vares, Bosnia & Herzegovina and Cheltenham, UK. And is managed by gDat data solutions in an acQuire database, which is regularly backed-up.

Discuss any adjustment to assay data.

No adjustments were necessary.

Location of data points

Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.

Sampling sites were surveyed using Total Station to better than 0.05m accuracy in the local BiH coordinate system.

Specification of the grid system used.

The grid system used MGI 1901 / Balkans Zone 6.

Quality and adequacy of topographic control.

The topographic surface of the immediate area was generated from a LiDAR survey to an accuracy of approximately 0.05m. It is considered sufficiently accurate for the Company's current activities.

Data spacing and distribution

Data spacing for reporting of Exploration Results.

Results from two drill holes are being reported. All samples were collected at 2m intervals down hole.

Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.

Drill hole spacing is deemed sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource classifications applied.

Whether sample compositing has been applied.

Sample composite was not employed.

Orientation of data in relation to geological structure

Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.

Reported holes were drilled at an average declination and azimuth as stated in Table 2 of the accompanying report.

The drill holes are considered to be reasonably orthogonal to the interpreted dip of the mineralisation, or close to it.

If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.

It is not considered that the drilling orientation has introduced a sampling bias, as the drilling is considered to be orthogonal to the strata bound mineralisation, or close to it.

Sample security

The measures taken to ensure sample security.

Chain of Custody of digital data is managed by the Company. Physical material was stored on site and, when necessary, delivered to the assay laboratory. Thereafter laboratory samples were controlled by the nominated laboratory. All sample collection was controlled by digital sample control file(s) and hard-copy ticket books.

Audits or reviews

The results of any audits or reviews of sampling techniques and data.

A Site and Laboratory (ALS and SGS, Bor) visit was made by Dr Belinda van Lente, an employee of CSA Global in January 2018. There were no material issues found for the 2017 drill campaign.

 

 

Section 2: Reporting of Exploration Results

(Criteria listed in the preceding section also apply to this section)

 

Criteria

JORC Code explanation

Commentary

Mineral tenement and land tenure status

Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.

The Rupice deposit is located within the Company's 100% owned Concession, No. 04-18-21389-1/13, located 13km west of Vares in Bosnia. There are no known material issues with any third party other than normal royalties due to the State.

The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.

The Concession is in good standing with the governing authority and there is no known impediment to the Concession remaining in force until 2038 (25 years), subject to meeting all necessary reporting requirements.

Exploration done by other parties

Acknowledgment and appraisal of exploration by other parties.

Modern exploration commenced with the work of Energoinvest in the late 1960s. During 1968-1969 underground development of 455m of drives and cross cuts were made, and 11 surface trenches dug for a total length of 93.5mm. Between 1980 and 1989, 49 holes were drilled for an advance of 5,690.8m. Sample material from all of these programs was routinely analysed for lead, zinc, and barite, and on occasion silver and gold. The deposit was the subject of a number of reserve estimates in the 1980s. This work is documented in many reports which are certified by those geoscientists and Institutes that undertook the work.

 

The work is considered to be of a standard equal to that prevalent within today's exploration industry.

Geology

Deposit type, geological setting and style of mineralisation.

The host rocks at Rupice comprises Middle Triassic limestone, dolostone, calcareous and dolomitic marl, and a range of mostly fine-grained siliciclastic rocks including cherty mudstone, mudstone, siltstone and fine-grained sandstone. The main mineralised horizon is a brecciated dolomitic unit that dips at around 50o to the northeast and has been preferentially mineralised with base, precious and transitional metals. The Triassic sequence and has been intensely deformed both by early stage ductile shearing and late stage brittle faulting.

The Rupice polymetallic mineralisation consists of sphalerite, galena, barite and chalcopyrite with gold, silver, tetrahedrite, boulangerite and bournonite, with pyrite. The majority of the high-grade mineralisation is hosted within the brecciated dolomitic unit, which is offset and cut by northwest striking, westerly dipping syn-post mineral faulting. This faulting displaces the mineralised body up to 20 metres in places. Thickening of the central portion of the orebody occurs where these faults flexure and deform. Mineralised widths up to 65 metres true thickness are seen in the central portion of the orebody.

To date, the massive sulphide mineralisation at Rupice has a defined strike length of 650 metres, with an average true-width thickness of around 20 metres. However, mineralisation at Rupice still remains open towards the north and down-dip to the south.

Drill hole information

A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:

o easting and northing of the drill hole collar

o elevation or RL (Reduced Level - elevation above sea level in metres) of the drill hole collar

o dip and azimuth of the hole

o downhole length and interception depth

o hole length.

If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.

167 diamond drill holes (38,134.65m) were used for the Mineral Resource estimate. This includes 46 historical holes (5,071.8m) not drilled by Adriatic Metals. All these holes were used to support the Mineral Resource estimate. The Mineral Resource estimate conveys the tenor of grade from the drill holes.

 Data aggregation methods

In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. cutting of high grades) and cut-off grades are usually Material and should be stated.

No data aggregation methods were applied.

Where aggregate intercepts incorporate short lengths of high-grade results and longer lengths of low-grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.

Not applicable as no data aggregation methods were applied.

The assumptions used for any reporting of metal equivalent values should be clearly stated.

Equivalent explanations are described in the body of the text.

Relationship between mineralisation widths and intercept lengths

These relationships are particularly important in the reporting of Exploration Results.

Exploration results are not being reported.

If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.

The majority of the high-grade mineralisation is hosted within the brecciated dolomitic unit, which is offset and cut by northwest striking, westerly dipping syn-post mineral faulting. This faulting displaces the mineralised body up to 20 metres in places. Thickening of the central portion of the orebody occurs where these faults flexure and deform. Mineralised widths up to 65 metres true thickness are seen in the central portion of the orebody.

To date, the massive sulphide mineralisation at Rupice has a defined strike length of 650 metres, with an average true-width thickness of around 20 metres. However, mineralisation at Rupice still remains open towards the north and down-dip to the south.

Recent drilling by Eastern Mining was mostly inclined at between 70o and 80 o to the southwest, perpendicular to the deposit strike, and intersected the mineralisation reasonably orthogonally.

If it is not known and only the downhole lengths are reported, there should be a clear statement to this effect (e.g. 'downhole length, true width not known').

True width intercepts in drill holes being reported are as follows -

BR-10-20 - 1.7m

BR-11-20 - 4.8m

BR-12-20 - 2.9m

BR-13-20 - 10.0m

BR-17-20 - 1.4m

BR-18-20 - 7.0m

BR-20-20 - 9.8m

BR-22-20 - 4.0m

BR-23-20 - 7.0m

Diagrams

Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.

Relevant maps and diagrams are included in the body of the report.

Balanced reporting

Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high-grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.

Not applicable. All mineralised incepts are being reported.

Other substantive exploration data

Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples - size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.

No substantive exploration data not already mentioned in the report has been used in the preparation of the Mineral Resource estimate.

Further work

The nature and scale of planned further work (e.g. tests for lateral extensions or depth extensions or large-scale step-out drilling).

Further drilling is being undertaken for geotechnical and hydrological purposes, and extension exploration drilling.

Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.

Diagrams have been included in the body of this report.

 

 

Section 3: Estimation and Reporting of Mineral Resources

(Criteria listed in section 1, and where relevant in section 2, also apply to this section)

 

Criteria

JORC Code explanation

Commentary

Database integrity

Measures taken to ensure that data has not been corrupted by, for example, transcription or keying errors, between its initial collection and its use for Mineral Resource estimation purposes.

Data used in the Mineral Resource Estimate was provided as a validated Micromine database, which in turn was sourced from a validated database prepared by Adriatic Metals. The validation routines were employed to confirm validity of data. Key files (collar, survey, geology, assay) were validated to ensure that they were populated with the correct original data.

All drill holes were logged to electronic logbooks. All drill hole collar, downhole survey and geological data are stored on the Virtual Cloud and at various locations including Vares, Bosnia & Herzegovina and Cheltenham, UK. And is managed by gDat data solutions in an acQuire database. The database is updated as new data become available.

Data validation procedures used.

The resultant database was validated for potential errors in Micromine software using specially designed processes.

The following error checks were carried out during final database creation:

· Missing collar coordinates.

· Missing values in fields FROM and TO.

· Cases when FROM values equal or exceed TO ones (FROM≥TO).

· Data availability. The data availability was checked for each drill hole in the tables:

- Collar coordinates

- Sampling data

- Downhole survey data

- Lithological characteristics.

· Duplicate drill hole numbers in the table of the drill hole collar coordinates.

· Duplicate sampling intervals.

· Duplicate downhole measurement data.

· Duplicate intervals of the lithological column.

· Sample "overlapping" (when the sample TO value exceeds FROM value of the next sample).

· Negative-grade samples.

Drill hole data was verified against source documentation. The surveyed drill holes were then also verified visually for consistency.

The Competent Person is satisfied that database integrity is appropriate to support Mineral Resource estimation.

Site visits

Comment on any site visits undertaken by the Competent Person and the outcome of those visits.

Phillip Fox is based on-site in Vares and was responsible for planning and implementation of the recent drilling programs, overseeing the preparation of the samples and their dispatch to the various laboratories. Mr. Fox assumes responsibility for the data components, QA/QC and geological interpretation. Dmitry Pertel assumes responsibility for the grade interpolation and reporting of the Mineral Resource estimate and has previously completed a site visit.

If no site visits have been undertaken, indicate why this is the case.

A site visit has been undertaken.

Geological interpretation

Confidence in (or conversely, the uncertainty of) the geological interpretation of the mineral deposit.

Sufficient drilling has been conducted to reasonably interpret the geology and the polymetallic mineralisation. The mineralisation is traceable between numerous drill holes and drill sections.

Interpretation of the deposit was based on the current understanding of the deposit geology. Each cross section generally spaced 20-30 m apart was displayed in Micromine software together with drill hole traces colour-coded according to grade values. The interpretation honoured modelled fault planes and interpretation of main geological structures. The mineralised structure of the deposit was interpreted and modelled using core logging data. The low-grade halo domain was interpreted to capture all mineralized samples, and based on the current understanding of the geological model. The fault zones were interpreted and modelled using geological logging. Cut-off grades for high grade domains were 10% for Zn, 3% for Pb, 25% for BaSO4, 1% for Cu, 2.5g/t for Au, and 110g/t for Ag. All cut-offs selected for interpretation were based on results of classical statistical analysis. The interpretation was independently reviewed by a consultant geologist.

Nature of the data used and of any assumptions made.

Geological logging in conjunction with assays has been used to interpret the mineralisation. The majority of holes were sampled at 2m intervals, with some more detailed sampling conducted.

The effect, if any, of alternative interpretations on Mineral Resource estimation.

Alternative interpretations are likely to materially impact on the Mineral Resource estimate on a local, but not global basis.

No alternative interpretations were adopted at this stage of the project.

The use of geology in guiding and controlling Mineral Resource estimation.

Geological logging in conjunction with assays and results of the statistical analysis has been used to interpret the mineralisation. Available historical maps and sections have been used to guide interpretation.

All internal waste was included into the interpreted mineralised bodies.

The factors affecting continuity both of grade and geology.

Continuity is affected by the nature of the host rocks, interpreted faults and limits of the drill holes.

The Competent Person is satisfied that the geological interpretation is appropriate to support Mineral Resource estimation.

Dimensions

The extent and variability of the Mineral Resource expressed as length (along strike or otherwise), plan width, and depth below surface to the upper and lower limits of the Mineral Resource.

The strike length is about 650m and width up to 250m. The combined thickness of the mineralised zones varies from several metres to 65m. Depth below surface is from 0 to 380 m, which is the lower limit of current drilling.

The Competent Person is satisfied that the dimensions interpreted are appropriate to support Mineral Resource estimation.

Estimation and modelling techniques

The nature and appropriateness of the estimation technique(s) applied and key assumptions, including treatment of extreme grade values, domaining, interpolation parameters and maximum distance of extrapolation from data points. If a computer assisted estimation method was chosen include a description of computer software and parameters used.

The Mineral Resource estimate was based on surface diamond drill core using ordinary kriging (OK) to form 5x5x5m blocks. The block model was constrained by wireframes modelled based on geology using sectional interpretation. Additional wireframing for each element for the high-grade domains within these geological wireframes (except for As, Sb and Hg) was completed. Weakly mineralised halos and fault zones used geological logging and multi-element assay data. The applied cut-off grades for high grade domains were:

 

Micromine software was used to generate the wireframes and for block modelling

Hard boundaries were used between mineralised lenses at each domain. The drill hole data were composited to a target length of 2m based on the length analysis of raw intercepts.

Geostatistical analysis was completed for all elements, and averaged long ranges were employed to justify the search ellipse - 102m along strike, 61m down dip and 31m across dip.

Interpolation parameters were:

Search pass 1: 2.5m by 2.5m by 2.5m. Minimum samples number - 1, minimum holes - 1, maximum samples number - 16.

Search pass 1: 1/3 of the variogram log ranges. Minimum samples number - 3, minimum holes - 2, maximum samples number - 16.

Search pass 2: 2/3 of the variogram log ranges. Minimum samples number - 3, minimum holes - 2, maximum samples number - 16.

Search pass 3: Full semi-variogram ranges. Minimum samples - 3, maximum samples - 16, minimum holes 2.

All subsequent search passes: incremented by full semi-variogram ranges in each direction. Minimum samples - 1, maximum samples - 16, minimum holes - 1.

Block discretisation 2*2*2.

The optimal parent cell size was selected in the course of block modelling based of 20x20m exploration drilling.

Classical statistical analysis was used to identify grade domains for barite, gold and silver.

The Competent Person is satisfied that estimation and modelling techniques are appropriate to support Mineral Resource estimation.

The availability of check estimates, previous estimates and/or mine production records and whether the MRE takes appropriate account of such data.

Previous JORC-compliant Mineral Resources were estimated by CSA Global in July 2019. The current estimate is about 32% higher in tonnage and about 22% lower grades due to the modelling methodology and domaining applied.

Mine production results were not available.

The assumptions made regarding recovery of by-products.

The Rupice deposit is a silver-gold-zinc-lead-barite deposit. Previous mining and beneficiation over a four-year period have shown that a conventional sulphide flotation method is a suitable recovery method. Metallurgical test work is ongoing to optimise the process flowsheet.

Estimation of deleterious elements or other non-grade variables of economic significance (e.g. sulphur for acid mine drainage characterisation).

As, Sb and Hg have been estimated in the model using their own semi-variogram models and OK interpolation method.

In the case of block model interpolation, the block size in relation to the average sample spacing and the search employed.

The average exploration drilling spacing was 20x20m. The selected parent cell size was 5x5m (quarter the exploration density). The search was based on the results of geostatistical analysis with average for all elements long ranges of 102x61x31m.

Any assumptions behind modelling of selective mining units.

No assumptions were made for selective mining unit, apart from the assumption that the deposit is likely to be mined by underground method and that 5x5m parent cell approximately reflects SMU for underground mining.

Any assumptions about correlation between variables.

Correlation between some variables was very strong (for example, between silver and lead), but no assumptions were made for the modelling purposes.

Correlation between bulk density and main elements (BaSO4, Pb, Zn and Cu) was used to calculate bulk density for all model domains except for the combined high-grade domain.

Description of how the geological interpretation was used to control the resource estimates.

Geological interpretation of the mineralised zone, weakly mineralised halo and fault zones was based on the geological logging. When grades within modelled wireframes for the mineralized zone had mixed populations, high-grade domain was modelled using cut-offs justified by statistical analysis.

High grade domains for each element were modelled individually, except for As, Sb and Hg, which did not demonstrate mixed grade populations within the modelled mineralized zone.

Discussion of basis for using or not using grade cutting or capping.

Classical statistical analysis was carried out for each element and each domain. It was found that histograms and probability plots did not demonstrate any apparent mixed populations within the limits of corresponding modelled domains. Top-cuts were identified and applied as shown in the table below:

 

The process of validation, the checking process used, the comparison of model data to drill hole data, and use of reconciliation data if available.

Grade estimation was validated using visual inspection of interpolated block grades versus underlying data, and swath plots.

Swath plots demonstrated reasonable correlation of modelled grades with the sample composites.

The Competent Person is satisfied that estimation and modelling techniques are appropriate to support Mineral Resource estimation.

Moisture

Whether the tonnages are estimated on a dry basis or with natural moisture, and the method of determination of the moisture content.

The tonnages were estimated on an in-situ dry bulk density basis which includes natural moisture. Moisture content was not estimated.

Cut-off parameters

The basis of the adopted cut-off grade(s) or quality parameters applied.

The reporting cut-off grade of 50g/t silver equivalent was supported by estimation of marginal cut-off for underground mining using input economic parameters and criteria.

The Competent Person is satisfied that cut-off parameters were appropriately considered, to support Mineral Resource estimation.

Mining factors or assumptions

Assumptions made regarding possible mining methods, minimum mining dimensions and internal (or, if applicable, external) mining dilution. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential mining methods, but the assumptions made regarding mining methods and parameters when estimating Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the mining assumptions made.

A scoping and on-going preliminary economic assessment studies were performed to ensure that there are reasonable prospects for the eventual economic extraction of the mineralisation, which demonstrated that the deposit is likely to be developed by underground mining method(s). Input parameters were provided by the Company as being typical for the commodity, mining method and costs for a Balkan silver-lead-zinc mining operation.

Metallurgical factors or assumptions

The basis for assumptions or predictions regarding metallurgical amenability. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential metallurgical methods, but the assumptions regarding metallurgical treatment processes and parameters made when reporting Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the metallurgical assumptions made.

A number of flotation tests have recently been carried out on both Rupice and Veovača (nearby deposit) bulk samples. Preliminary results indicate there is potential to produce Zn, Pb/Cu and barite concentrates via flotation processes, with good recoveries of all constituents reported in this Mineral Resource estimate.

The test work also indicates that a barite product that meets market specification requirements of purity, specific gravity, and fineness of particle size can be achieved, which meets the requirements of Clause 49 of the JORC Code.

This test work remains ongoing.

The Competent Person is satisfied that metallurgical factors and assumptions were appropriately considered, to support Mineral Resource estimation.

Environmental factors or assumptions

Assumptions made regarding possible waste and process residue disposal options. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider the potential environmental impacts of the mining and processing operation. While at this stage the determination of potential environmental impacts, particularly for a greenfield project, may not always be well advanced, the status of early consideration of these potential environmental impacts should be reported. Where these aspects have not been considered this should be reported with an explanation of the environmental assumptions made.

No detailed assumptions regarding possible environmental impacts to the site area were considered. The general locality has a number of active mining operations and no environmental impediments are anticipated.

Bulk density

Whether assumed or determined. If assumed, the basis for the assumptions. If determined, the method used, whether wet or dry, the frequency of the measurements, the nature, size and representativeness of the samples.

Bulk densities were determined on drill core every 2m in ore and every 5m in waste. At total of 5,864 determinations were used to calculate regression formulas using barite, lead zinc and copper grades vs bulk density or to interpolate bulk density values into the combined high-grade domain.

The bulk density for bulk material must have been measured by methods that adequately account for void spaces (vugs, porosity, etc), moisture and differences between rock and alteration zones within the deposit.

Bulk density determinations adopted the weight in air / weight in water method using a suspended or hanging scale. First the core billet was accurately weighed dry ("in air"), the core billet was removed, and the wire cage fully submerged in water and its tare set to "zero" mass. The billet of core was then fully submerged and weighed ("weight in water"). The bulk density is calculated by the formula BD = Md / Md - Mw, where Md = weight in air and Mw = weight in water.

Discuss assumptions for bulk density estimates used in the evaluation process of the different materials.

No assumptions were made for Bulk Density.

The Competent Person is satisfied that density was appropriately considered, to support Mineral Resource estimation.

Classification

The basis for the classification of the Mineral Resources into varying confidence categories.

Resource classification was based on confidence in the QA/QC data analysis, geological interpretation, drill spacing, geostatistical measures, a visual evaluation of cross sections and drill density, and manual interpretation of resource categories. The interpreted boundaries between categories were wireframed and used to code the block models. Generally, the Indicated category was assigned to the areas with reasonable continuity of mineralised lodes based on 20x20m and 40x40m exploration drilling. All other blocks were classified as Inferred. No blocks were classified as Measured

Whether appropriate account has been taken of all relevant factors (i.e. relative confidence in tonnage/grade estimations, reliability of input data, confidence in continuity of geology and metal values, quality, quantity and distribution of the data).

The classification has taken into account all available geological and sampling information as well as the structural information, and the classification level is considered appropriate for the current stage of this project.

Whether the result appropriately reflects the Competent Person's view of the deposit.

The Mineral Resource estimate appropriately reflects the view of the Competent Person.

The Competent Person is satisfied that classification of this Mineral Resource estimate appropriately reflects the data and interpreted geological controls on mineralisation.

Audits or reviews

The results of any audits or reviews of MREs.

The current model has not been audited by an independent third party but has been subject to CSA Global's internal peer review processes.

Discussion of relative accuracy/ confidence

Where appropriate a statement of the relative accuracy and confidence level in the MRE using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the resource within stated confidence limits, or, if such an approach is not deemed appropriate, a qualitative discussion of the factors that could affect the relative accuracy and confidence of the estimate.

Industry standard modelling techniques were used, including but not limited to:

· Classical statistical analysis, cut-offs selection.

· Interpretation and wireframing.

· Top-cutting and interval compositing.

· Geostatistical analysis.

· Block modelling and grade interpolation techniques.

· Model classification, validation and reporting.

The relative accuracy of the estimate is reflected in the classification of the deposit.

The relative accuracy of the Mineral Resource estimate is reflected in the reporting of the Mineral Resource to an Indicated and Inferred classification as per the guidelines of the 2012 JORC Code.

The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used.

The statement refers to global estimation of tonnes and grade and is suitable for use in a subsequent PFS and further exploration at the deposit.

These statements of relative accuracy and confidence of the estimate should be compared with production data, where available.

No production data is available.

The Competent Person is satisfied that classification of this Mineral Resource estimate appropriately reflects the data and interpreted geological controls on mineralisation.

 

 

 

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