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Resource Statement

28 Aug 2008 10:11

RNS Number : 1897C
Niger Uranium Limited
28 August 2008
 



For immediate release

28 August 2008

NIGER URANIUM LIMITED

("Niger Uranium" or "the Company")

Resource Statement

The Board of Niger Uranium is pleased to announce its maiden resource statement for the Company's IN GALL Target on the IN GALL Property in Niger.

Highlights

·; Niger Uranium is pleased to announce a SAMREC compliant Inferred Resource of 4.39 million lbs eU3O8 at the In Gall target on the company’s 100% owned In Gall license.
 
·; This maiden resource estimate of 14.06 million tonnes at an average grade of 141.5 ppm eU3O8 using a 100 ppm cut-off (containing 4.39 Mlbs eU3O8) was completed by MSA Geoservices of Johannesburg, based upon 2,664.7 metres of drilling in 58 boreholes drilled on a 250 by 500 metre grid.
 
·; The mineralisation is open; the host-formation has been followed westwards by Niger Uranium for 16 kilometres along strike and up to 10 kilometres in width by limited trenching and shallow drilling.
 
·; This target is in the southern portion of the IN GALL license, one of 8 licenses held by the Company in Niger covering a total of 6,773 square kilometers; all are located in the Tim Mersoi Basin, the world’s 5th largest uranium producing district.
 

The In Gall Resource

MSA declares the following SAMREC compliant Inferred Resources at Ingall at varying cut off grades:

Cut off grade 

(ppm eU3O8)

Inferred Resource 

(Million tonnes)

Grade 

(ppm eU3O8)

Metal 

(million lbs eU3O8)

50

48.09

92.0

9.76

75

27.84

114.3

7.02

100

14.06

141.5

4.39

125

6.55

176.3

2.55

The uranium at In Gall is associated with an extensive disconformity between the Cretaceous-aged Tegama and Irhazer arenaceous formations. This disconformity crops out at surface and is generally flat lying. The mineralised layer is typically 0.2 to 2.3 metres thick and continuous; within the resource area every borehole intersected mineralisation above a minimum 20 centimetre-100 ppm eU3O8 cut-off. A single minor fault has been identified transecting the zone of mineralisation, but is not expected to have a material impact on the resource estimate.

Mineralogical work on borehole samples has been completed by SGS of Johannesburg. Carnotite, uranophane+/- coffinite and autinite were identified by SEM work as the main uranium bearing phases, typically within a silicate gangue. 

All boreholes are vertical and drilled by the tri-cone method and probed using a Robertson Geologging gamma tool. The probe was calibrated by Medusa Systems BV in the Netherlands, to provide equivalent uranium grades expressed as eU3O8. To support the probe data, 5 diamond core holes were drilled to twin 5 tri-cone holes across the resource area. Samples were collected at 0.2 metre intervals through the mineralised layer and analysed for U3O8 by XRF. The results support the equivalent uranium grades used in the resource estimate. These results are contained in appendix 1

The resource is open; the host-formation has been followed westwards by Niger Uranium for 16 kilometres along strike by limited trenching and shallow drilling. Once the rainy season is over (October) step out drilling to extend the resource is planned. 

Where the mineralised layer is exposed at surface, trenches have been excavated to provide exposures to assist with the understanding of the mineralised material. Specific gravity measurements on five samples completed by SGS gave a narrow range of 2.56 to 2.74; an average density of 2.65 tonnes/cubic metre was used for the resource estimate.

Resource estimation and categorisation of the grade estimate was undertaken on the basis of the criteria laid out in the South African SAMREC code. The estimate was made in Datamine. Inverse distance-squared interpolation was used to estimate eU3O8 grades into blocks with dimensions of 50 m (easting), 50 m (northing) and 0.5 m (RL). The search ellipsoid dimensions chosen for the grade interpolation process were 500 m in Easting and Northing and 0.5 m in RL, within the defined envelope.

MSA believes the status and magnitude of these resources could be raised by step-out and infill drilling to further define and possibly extend the known strike length of the high-grade channel. Additional density measurements are also required. All additional and the earlier 2008 drillholes should be accurately collar-surveyed to confirm data integrity. 

Work Programme

In addition to work at the In Gall target, the company is gearing up for the field season commencing late September. Step-out holes are planned to be drilled at the Aboye target where a single borehole (AB003) drilled early in 2008 returned 9 metres at 125 ppm eU3O8 (reported previously) within the Tchirezrine II formation, the formation that hosts Areva's massive Imouraren deposit. 

At other targets within the Irhazer and In Gall licenses a 1600 point radon and geochemical survey is planned given the possible improvement in the security situation in Northern NigerThis survey will be carried out over the favorable structural corridors along which numerous airborne anomalies and anomalous grab samples have been collected (reported previously). The radon data should detect potential concealed uranium mineralisation. In addition, conventional soil and rock analyses will be carried out at each point, to provide a fully integrated geochemical database, which will be used to define target areas for follow-up sampling and drill testing. 

John Sanders, Director and CEO said:

"The In Gall target is the 3rd area to be tested by the company in just over 6 months of operation; the fact that a new uranium resource has been discovered so early in our exploration programme is an excellent result. As well as extending and upgrading this resource, work will now shift to the other high priority targets where every effort will be made to repeat the exploration success achieved at In Gall."

Mr. Richard Wadley (Pr. Sci. Nat), Senior Consultant at MSA Geoservices, is the qualified person responsible for Niger and has verified the data reported above. Mr Wadley is a consultant to Niger Uranium, with no interest in the Company and has consented to the inclusion in this announcement of his name in the form and context in which it appears. Exploration data is acquired by Niger Uranium using best practice quality assurance and quality control protocols. 

For further information:

Niger Uranium Limited John Sanders, Chief Executive Officer

Gordon Cassidy, Finance Director

Tel: +27 (0)11 269 4900

Beaumont Cornish Limited

Michael Cornish 

Tel: + 44 (0) 20 7628 3396

Forward-Looking Statements:

This press release contains statements that are 'forward-looking'. Generally, the words 'expect,' 'intend,' 'estimate,' 'will' and similar expressions identify forward-looking statements. By their very nature, forward-looking statements are subject to known and unknown risks and uncertainties that may cause our actual results, performance or achievements, or that of our industry, to differ materially from those expressed or implied in any of our forward-looking statements. Statements in this press release regarding the Company's business or proposed business, which are not historical facts, are 'forward looking' statements that involve risks and uncertainties, such as estimates and statements that describe the Company's future plans, objectives or goals, including words to the effect that the Company or management expects a stated condition or result to occur. Since forward-looking statements address future events and conditions, by their very nature, they involve inherent risks and uncertainties. Actual results in each case could differ materially from those currently anticipated in such statements. These forward-looking statements speak only as of the date they are made.

  

Appendix 1.

Results of diamond core verification analyses by XRF and probe results for the same intervals for the original and 'twin' holes. Analyses were completed by SGS Lakefield Laboratory, South Africa.

Borehole Number

Depth (metres)

Sample

Original Hole eU3O8 (ppm)

Twin Hole eU3O8 (ppm)

XRF U3O8 (ppm)

From

To

H17

30A

26.30

26.50

602

17

30

10

H17

30A

26.50

26.70

603

21

30

20

H17

30A

26.70

26.90

604

27

47

40

H17

30A

26.90

27.10

606

44

75

50

H17

30A

27.10

27.30

607

88

115

210

H17

30A

27.30

27.50

609

199

190

50

H17

30A

27.50

27.70

612

279

240

340

H17

30A

27.70

27.90

613

167

178

310

H17

30A

27.90

28.10

614

100

113

140

H17

30A

28.10

28.30

616

65

67

50

H17

30A

28.30

28.50

617

43

43

30

H17

30A

28.50

28.70

619

31

30

20

H17

30A

28.70

28.90

622

29

29

20

H17

30A

28.90

29.10

623

30

27

30

H17

60B

39.70

39.90

624

28

25

20

H17

60B

39.90

40.10

626

35

26

20

H17

60B

40.10

40.30

627

45

33

40

H17

60B

40.30

40.50

629

53

46

20

H17

60B

40.50

40.70

632

87

62

40

H17

60B

40.70

40.90

633

232

165

40

H17

60B

40.90

41.10

634

275

327

50

H17

60B

41.10

41.30

636

159

226

410

H17

60B

41.30

41.50

637

89

119

200

H17

60B

41.50

41.70

639

57

70

50

H17

60B

41.70

41.90

642

41

44

20

H17

60B

41.90

42.10

643

29

35

10

H17

60B

42.10

42.30

644

24

28

10

H17

57DE

46.70

46.90

646

36

43

40

H17

57DE

46.90

47.10

647

38

47

40

H17

57DE

47.10

47.30

649

42

55

60

H17

57DE

47.30

47.50

652

59

58

60

H17

57DE

47.50

47.70

653

77

65

70

H17

57DE

47.70

47.90

654

165

98

100

H17

57DE

47.90

48.10

656

246

171

210

H17

57DE

48.10

48.30

657

295

246

180

H17

57DE

48.30

48.50

659

339

408

920

H17

57DE

48.50

48.70

662

369

302

250

H17

57DE

48.70

48.90

663

247

169

190

H17

57DE

48.90

49.10

664

118

94

20

H17

57DE

49.10

49.30

666

77

58

20

H17

57DE

49.30

49.50

667

63

54

50

H17

57DE

49.50

49.70

669

59

52

20

H17

57DE

49.70

49.90

672

59

43

30

H17

57DE

49.90

50.10

673

61

43

40

H17

55E

56.75

56.95

674

21

24

30

H17

55E

56.95

57.15

676

15

18

20

H17

55E

57.15

57.35

677

17

17

20

H17

55E

57.35

57.55

679

28

24

20

H17

55E

57.55

57.75

682

65

52

20

H17

55E

57.75

57.95

683

137

99

60

H17

55E

57.95

58.15

684

184

177

150

H17

55E

58.15

58.35

686

253

192

130

H17

55E

58.35

58.55

687

244

264

250

H17

55E

58.55

58.75

689

127

168

420

H17

55E

58.75

58.95

692

72

95

60

H17

55E

58.95

59.15

693

44

61

30

H17

55E

59.15

59.35

694

37

42

20

H17

55E

59.35

59.55

696

37

36

20

H17

55E

59.55

59.75

697

34

33

20

H17

55E

59.75

59.95

699

32

35

20

H17

50G

48.70

48.90

702

36

36

30

H17

50G

48.90

49.10

703

34

34

50

H17

50G

49.10

49.30

704

34

34

30

H17

50G

49.30

49.50

706

38

38

40

H17

50G

49.50

49.70

707

55

55

100

H17

50G

49.70

49.90

709

94

94

140

H17

50G

49.90

50.10

712

190

190

270

H17

50G

50.10

50.30

713

291

291

310

H17

50G

50.30

50.50

714

229

229

170

H17

50G

50.50

50.70

716

190

190

80

H17

50G

50.70

50.90

717

132

132

30

H17

50G

50.90

51.10

719

77

77

30

H17

50G

51.10

51.30

722

48

48

20

H12

50G

51.30

51.50

723

40

40

20

H12

50G

51.50

51.70

724

34

34

30

H12

50G

51.70

51.90

726

31

31

20

Appendix 2.

Glossary

Uranium

Uranium is a silver grey moderately radioactive metallic element that has the symbol U and an atomic weight of 238.03

In-situ leaching (ISL)

In-situ leaching (ISL) or solution mining is a process of recovering minerals such as copper and uranium through boreholes drilled into the deposit. Explosive or hydraulic fracturing may be used to create open pathways in the deposit for a solution to penetrate. Leaching solution is pumped into the deposit where it makes contact with the ore. The solution bearing the dissolved ore content is then pumped to the surface and processed.

Tri-cone drilling

A rapid, relatively cost effective technique of drilling boreholes for uranium exploration by gamma ray probe. The tri-cone drill (or roller) bit, consists of three cone shaped toothed rollers in a cluster. Each of the cones has hard teeth mounted on bearings. The spatial control of sampling for laboratory purposes is not good with tri-cone drilling and alternative drilling techniques would have to be used.

CR39 radon survey

Is a technique of soil survey to measure or detect buried uranium mineralization in certain geological environments.

U3O8

eU3O8

The uranium content of a sample is reported as U3O8 if the analysis is performed in a laboratory. Uranium content when measured by a gamma ray down hole probe is reported as eU3O8.

XRF

X-ray Fluorescence Analysis is a sophisticated laboratory technique for the analysis of uranium and other elements

BHID

Abbreviation for borehole identification number.

UTM

Abbreviation for Universal Transverse Mercator which is a grid-based coordinate system method of specifying locations on the surface of the Earth.

Borehole Collar

The surveyed starting point of a borehole at the earth's surface

ppm

Abbreviation for parts per million. 1000 parts per million are equivalent to 0.1%

ENDS

This information is provided by RNS
The company news service from the London Stock Exchange
 
END
 
 
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