Cora Gold Regulatory News (CORA)

Drilling type

No. of holes

Total metres (m)

Minimum length (m)

Maximum length (m)

Average length (m)

RAB

367

7,757

1

26

21

AC

281

20,065

16

119

71

RC/ACRC

628

65,172

24

180

104

DD/RCDD/ACDD

45

6,840

29

300

152

AUG

AC

ACDD

ACRC

DD

PIT

RAB

RC

RCDD

Zone B

2

2

4

1

9

3

21

Selin

3

4

1

40

1

49

Zone A

8

1

37

3

49

Zone B North

32

32

Zone A&C extension

23

55

3

22

16

1

120

Selin Bokoro-East extension

56

22

18

96

Bokoro-West

4

8

1

13

Target 3

17

52

6

75

Target 5 & Target 6

5

53

9

67

Dako-Main

40

6

46

Zone C

8

1

8

17

Fode 1

6

2

8

Selin

 1.4

 1.9

0.60

1.19

Zone B

0.9

1.2

0.62

1.39

Zone A

0.6

0.8

0.55

1.22

Zone C

0.4

0.6

0.56

0.93

Zone B N

0.2

0.3

0.60

0.94

Sub-Total MRE Areas

3.6

4.9

0.59

1.20

70

 190

Target 3

5.9

8.0

0.60

1.20

Target 5 and 6

4.7

6.4

0.53

1.09

Selin Bokoro W extension

4.1

5.6

0.55

1.29

Zone A and C ext

3.5

4.8

0.55

1.09

Dako Main

2.6

3.5

0.60

1.29

Fode 1

0.9

1.2

0.77

1.99

Bokoro W

0.7

0.9

0.76

1.06

Sub-Total outside MRE

22.4

30.4

0.58

1.21

 420

 1,180

TOTAL

26.0

35.2

0.58

1.21

 490

 1,370

Bert Monro

Craig Banfield

Cora Gold Limited

info@coragold.com

Christopher Raggett / Charlie Beeson

finnCap Ltd

(Nomad & Joint Broker)

+44 (0) 20 7220 0500

Andy Thacker

James Pope

Turner Pope Investments

(Joint Broker)

+44 (0) 20 3657 0050

Susie Geliher / Charlotte Page

St Brides Partners

(Financial PR)

pr@coragold.com

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 downhole gamma sondes, or handheld XRF instruments, etc.). These examples should not be taken as limiting the broad meaning of sampling.

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

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.

The Mineral Resource estimate (MRE) is based on reverse circulation (RC) chip and diamond drill core sampling. The 2021/2022 program was composed of 48,090 m of RC and 3,894 m of diamond drilling (DD).

The Exploration Target is based on all available drilling, regardless of type. 3363 drillholes were considered for the Exploration Target and a total of 593 drillholes were used.

RC was ubiquitously sampled on 1 m intervals. Each rod string is 6 m in length and is checked and marked with grease every 1 m to allow personnel to observe sampling and drill progress. The driller will sound a horn at the end of each 1 m interval, warning the samplers to switch bags at the cyclone.

All industry standard RC sample quality procedures were applied, and each shift a geologist was present to ensure sample quality was maintained, holes were not stopped in mineralisation and activity reporting monitored cost control. No detailed logging or sampling was conducted at the rigs.

All bulk 1 m samples were transported immediately upon hole completion to a central bag farm next to the Sanankoro camp. No samples were left in the field. All samples drilled were shipped to the bag farm for splitting and logging under controlled and secured conditions.

The 1 m bulk samples are riffle split down to 5-6 kg using a three-tier 75:25 riffle splitter and a duplicate pair of 2-3 kg samples are then generated using a two-tier 50:50 riffle splitter. One sample is sent to the lab and the duplicate is stored for any future re-assay or reference.

All RC holes are photographed on chip tables and chip trayed after sampling and logging.

All RC holes are geologically logged and panned for visible gold on1 m intervals concurrently with sampling.

The logging and panning results dictate whether the logging or senior geologist will instruct compositing in less favourable intersections of a hole. Composites of 4 m are possible in barren intersections.

Sampling of DD core aims to maintain a standard 1 m interval but can be sampled from 0.5 m to 1.5 m in length, depending upon the interval required to reach the mineralised contact or select the vein width.

All core is saw cut. Sample interval ends are saw cut pre-sampling to ensure sampling intervals are adhered to.

All core boxes are metal.

All core boxes are photographed wet and dry upon receipt at the core shed from the rig.

The RC samples were sent to an accredited laboratory where they were pulverised to 85% passing 75 micron in a Labtechnics LM2 puck pulveriser and sub-sampled to provide 2 kg for CN Bottle Roll and/or a 50 g aliquot for fire assay. Bottle roll is the preferred assaying method for oxide materials and fire assay for fresh or sulphide-rich material.

Rotary air blast (RAB), aircore (AC) and AC hammer were sampled and analysed as per the RC procedure.

The DD samples are sent to an accredited laboratory where they were jaw-crushed 95% passing 2 mm, then pulverised down to 85% passing 75 micron in an Labtechnics LM2 puck pulveriser and subsampled to provide 2 kg for CN Bottle Roll and/or a 50 g aliquot for fire assay. Bottle roll is the preferred assaying method for oxide materials and fire assay for fresh or sulphide-rich materials.

Vertical auger drilling was conducted to gain a sample of the interface material below transported surface gravels. Auger holes ranged from 0.5 m to 5.0 m and were sent to an accredited laboratory where they were pulverised to 85% passing 75 micron in a Labtechnics LM2 puck pulveriser and subsampled to provide 2 kg for CN Bottle Roll and or a 50 g aliquot for fire assay. Bottle roll is the preferred assaying method for oxide materials and fire assay for fresh or sulphide-rich material.

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.).

Various drilling techniques have been used at Sanankoro - auger, RAB, AC, AC hammer, RC, and diamond DD.

The database was flagged as two parts, an exploration database consisting of auger, RAB, AC and AC hammer; and a Mineral Resource database consisting of RC and DD.

All 2021 core intervals are orientated using a WELLFORCE DV8 iCORE ORI instrument when geologically possible.

DD core was drilled on an average of 3 m rod pulls but depending upon ground conditions 1.5 m or 6 m rod pulls could have been applied. PQ was used through the soft, friable oxide from surface normally to between 40 m and 80 m. The drill string was reduced subsequently to HQ. NQ was not drilled in 2021.

RC was drilled using a 53/8" face-sampling hammer

All drilling details and dates are recorded on hole logs and are stored in the COLLAR file on DATASHED™.

Drill sample recovery

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

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.

DD core was drilled on an average of 3 m rod pulls but depending upon ground conditions 1.5 m or 6 m rod pulls could have been applied. PQ was used through the soft, friable oxide from surface normally to between 40 m and 80 m. The drill string was reduced subsequently to HQ. NQ was not drilled in 2021.

DD core recoveries were estimated on industry standard methods of direct tape measure on core reconstructed on a triple-length angle-iron cradle, locked where possible and corrected for stick-up errors.

RC was drilled using a 5 3/8" face-sampling hammer leading a 41/2" standard rod string. Auxiliary booster-compressor air packs were used on deeper holes, normally > 110m, to ensure dry sample quality and recovery.

The RC drilling was sampled on a standard 1 m interval and recoveries assessed quantitively by weighing each sampled metre. The practice of weighing drill chip samples immediately from recovery at the rig is Cora Gold Limited (Cora Gold) standard practice for all RAB, AC and RC drilling.

Sample quality and recovery are monitored at the rig during drilling shift both observationally by the geologist checking the moisture content, possible contamination and relative recovery along the bag line and quantitively by weighing each of the bulk 1 m samples direct from the cyclone before layout.

DD and RC recoveries are logged and recorded in the database. Overall recoveries are >90% for the DD and >70% for the RC; there are no core loss issues or significant sample recovery problems. A geologist is always present at the rig to monitor and record sample quality.

The Mineral Resource is defined by DD and RC drilling, which have high sample recoveries. No relationship between sample recovery and grade have been identified at the project. The consistency of the mineralised intervals and density of drilling is considered to preclude any issue of sample bias due to material loss or gain.

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.

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

The total length and percentage of the relevant intersections logged.

All RC holes are logged, panned and sampled on a standard 1 m resolution. Every 1 m drilled is logged and panned before being sampled.

4 m compositing may be instructed in barren sections of drilled hole based on the results of the detailed logging.

All RC holes are photographed on chip tables and chip trayed after sampling and logging.

All DD core is transported to the core shed located at the main Sanankoro Camp for full rock quality designation (RQD), geotechnical logging and density/point load testing determinations prior to being released for geological logging and sampling from top to bottom of hole.

All core boxes are photographed wet and dry upon receipt at the core shed from the rig.

The level of detail in the logging is deemed appropriate for Mineral Resource estimation and reporting.

Subsampling techniques and sample preparation

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

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

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

Quality control procedures adopted for all subsampling stages to maximise representivity of samples.

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.

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

All RC chip samples were weighed and riffle split to 2-3 kg for submission to the lab. All RC holes are sampled in bulk, logged and panned on a standard 1 m interval. Compositing to 4 m may occur in barren geology.

All DD core is saw cut and half core sampled. DD sample intervals can range from 0.5 m to 1.5 m, depending on geology.

A standard 5:25 sample QAQC was used throughout 2021 and 2022, composed of one standard, one blank, two duplicates, and one triplicate. The 2021 and 2022 assay stream had a routine 20% QAQC component.

The database manager monitors all sampling and QAQC vetting of the assay stream.

Field duplicates assist in determining the representivity of subsamples.

Subsamples are deemed appropriate for Mineral Resource estimation and reporting.

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.

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.

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.

Sample preparation involved oven drying, jaw crushing core P70 passing 2 mm, followed by total pulverisation through an LM2 puck pulveriser to a nominal 85% passing 75 microns.

Historically it has been proven that the nuggety, highly weathered nature of the Sanankoro oxide mineralisation is best head assayed by 2 kg Bottle Roll/atomic absorption spectrometry (AAS) with a 50 g Fire Assay/AAS on the BR tail residue. The bulk of the MRE assay database is completed by this method.

The fresh sulphide mineralisation is assayed by standard total fusion 50 g Fire Assay/AAS.

A standard 5:25 sample QAQC was used throughout 2021 and 2022, composed of one standard, one blank, two duplicates, and one triplicate. The 2021 and 2022 assay stream had a routine 20% QAQC component.

Certified reference material (CRM) standards were sourced from accredited suppliers Geostats Pty Ltd and Rocklabs. CRM standards were used ranging from 0.1 ppm to 78.81 ppm.

Following review of the QAQC, the data are deemed appropriate for Mineral Resource estimation and reporting.

The Exploration Target is informed by Cora Gold drillholes and historical holes (pre-Cora Gold). The historical holes have no quality control results available.

Verification of sampling and assaying

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

The use of twinned holes.

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

Discuss any adjustment to assay data.

The Competent Person has visually verified significant intersections in DC and RC drilling during the site visit.

Geology and sampling data were logged into Microsoft Excel format templates and sent via email to the database manager. Files were imported into Datashed via configured importers and passed through stringent validation.

Validation included:

●  Logging codes checked against approved code lists

●  Interval overlaps and gaps

●  Records beyond end-of-hole.

All digital files received were archived on the workstation hosting the database. This was located on site with the database manager. Scheduled daily backups of the database and file archive were made to a NAS solution located at the same site. Nightly scheduled offsite backups were conducted to a verified backup service provider. All offsite backups are encrypted.

During the 2021 MRE drill program, historical Gold Fields Ltd (Gold Fields) RC and DD intercepts were twinned, along with previous Cora AC and RAB intercepts and previous important DD intercepts which correlated with sections of poor DD core recoveries.

The Gold Fields twin holes correlated closely, underwriting the use of the Gold Fields Mineral Resource data in the MRE where it is required.

Overall, the drilling, logging, sampling, assaying and QAQC procedures are considered to be consistent with industry standard practice.

No adjustments or calibrations were made to any assay data used in the estimates of the Mineral Resource and Exploration Target.

Location of data points

Accuracy and quality of surveys used to locate drillholes (collar and downhole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.

Specification of the grid system used.

Quality and adequacy of topographic control.

Grid System: WGS84 UTM zone 29N (EPSG: 32629)

All surface survey features were surveyed with a Leica GS18-T RTK differential global positioning system (GPS) to within a proven accuracy of 30 cm; Cora conducted the differential GPS work. All new and historical Mineral Resource drill collars were located and resurveyed by CG-Leica in 2021.

A large number of well distributed ground control points and features were used for the Terrabotics satellite survey. All points were set-out or picked-up using CG-Leica.

Terrabotics UK produced a site specific 139km2 digital terrain model (DTM) with 0.3 m RL accuracy using tasked Maxar orthorectified Worldview-3 (WV3) imagery flown in November to December 2020. The DTM was provided in February 2021 and utilised throughout the 2021 and 2022 drilling campaigns.

The Terrabotics DTM proved accurate from ongoing survey work to be within 30-50 cm RL. Differential GPS easting and northing showed better resolution.

The Terrabotics DTM is an acceptable topographic model for Sanankoro which defines the surface relief and maps the artisanal pits across the 139km2 area of interest accurately. The WV3 imagery maps the full cadastral and natural features across the project area.

The 2021 and 2022 drilling utilised a WELLFORCE CHAMP north-seeking gyro throughout and every drilled RC and DD hole has a detailed gyro DTH survey file. Historically, DTH surveys where conducted, used a REFLEX EZ-TRAC.

The 2021 DD utilised a WELLFORCE DV8 iCORE ORI orientation tool.

Topography for the Exploration Target was extended from data sourced from the United States Geological Survey website.

Data spacing and distribution

Data spacing for reporting of Exploration Results.

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.

Whether sample compositing has been applied.

The nominal drillhole collar spacing is 50 m x 25 m and 50 m x 50 m.

Due to the orientation of drill traces on section, data between drillholes can be spaced as close as 10 m in places.

The mineralised domains have demonstrated sufficient continuity in both geology and grade to support the definition of Inferred and Indicated Mineral Resources as per JORC 2012 guidelines.

The Exploration Target drillhole spacing varies within each area. The drilling was spaced between 50 m and 500 m in a north-south direction and 25 m to 200 m in an east-west direction.

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.

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.

The bulk of the drilling is orientated 090° or 270° orthogonal to the strike of the mineralised domains. Structural logging based on oriented core indicates that the main mineralisation controls are ±20° from 000° north and largely perpendicular to drill direction.

No orientation-based sampling bias has been identified in the dataset.

Sample security

The measures taken to ensure sample security.

The full chain of custody is managed by Cora. Samples collected daily from the rigs and transported to the central bag farm and sample processing area next to the main Sanankoro camp where the bulk samples are logged, split and prepared for onward transport to the various labs.

The samples are stored on site and a truck collects available samples weekly and transports them to Cora Gold office in Bamako for registration and verification prior to onward delivery to either SGS Ouagadougou or ALS Ouagadougou.

The labs sign sample submissions as evidence of receipt.

Completed assay files and pdf certificates were distributed to the approved recipients by Lab LIMS. Assay files were imported as received to Datashed and then archived on the workstation hosting the database.

Database management software used is DATASHED version 4.6.4.2 with DB version 4.6.5 with MSSQL Server SQL2017 backend.

Audits or reviews

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

Cora's Head of Exploration (at the time) visited each of the labs in November and December 2020 before signing contracts. No issues were identified during the visit.

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

The Sanankoro Gold Project (area 341.87km2) is located in the Yanfolila Gold Belt of southern Mali. The Sanankoro Gold Project comprises five contiguous gold exploration permits, being Bokoro II (area 63.1km2; expiry date 25 August 2023), Bokoro-Est (area 100km2; expiry date 18 September 2028), Dako II (area 44.66km2; expiry date 31 December 2027), Kodiou (area 50km2; expiry date 15 May 2023), and Sanankoro II (area 84.11 km2; expiry date 2 March 2030). The Definitive Feasibility Study is focused on Mineral Resources within the Sanankoro II gold exploration permit.

Cora Resources Mali SARL is a wholly owned subsidiary of Sankarani Ressources SARL which in turn is a 95% subsidiary of Cora Gold Limited. Sankarani Ressources SARL is registered in the Republic of Mali. Cora Gold Limited is registered in the British Virgin Islands. The residual 5% interest in Sankarani Ressources SARL may be acquired from a third party for the sum of US$1 million. In addition, the Sanankoro II permit is subject to a third party 1% net smelter return (NSR) royalty. All fees due to the government in respect of the Sanankoro II gold exploration permit have been paid and the permit is in good standing.

A gold exploration permit over the same area as that covered by the Sanankoro II gold exploration permit was previously held by Sankarani Resources SARL. This permit expired on 1 February 2020, having been initially awarded on 1 February 2013.

Exploration done by other parties

Acknowledgment and appraisal of exploration by other parties.

Exploration activities on the original Sanankoro permit by previous workers have included geological mapping, rock chip sampling, termite sampling, trench sampling geophysical surveys and surface drilling - auger, RAB, AC, RC, and DC.

There were two previous companies who conducted work at Sanankoro, i.e. Randgold Resources Ltd (Randgold) between 2004 and 2008 and Gold Fields between 2008 and 2012.

During 2004 to 2008, Randgold conducted successive programs of soils and termites geochemical sampling on iterative 500 m, 200 m and 100 m grids. Broad blocks of gradient array induced polarisation (IP) were completed to assist drill targeting on the broad regional-scale surface anomalies. They drilled broad spaced 400 m x 100 m auger and RAB fences in search for bedrock targets.

During 2008 to 2012, Gold Fields conducted infill soils and termite sampling down to 100 m x 25 m resolution. They conducted large blocks of regional gradient array IP and three main phases of drilling ranging from 400 m x 100 m RAB with follow-up AC down to50 m x 25 m RC and RC with DC tails, dependent upon results discovered.

Cora acquired the Sanankoro Permit in April 2017 and started exploration termite sampling in May 2017.

Geology

Deposit type, geological setting, and style of mineralisation.

Sanankoro is located on the leading western edge of the Yanfolila-Kalana Volcanic Belt, which is the western-most expression of the cratonic Baoulé-Mossi domain, on the major transcrustal margin with the Siguiri Basin. There is major deep-seated architecture across the district which links the major gold mines at Siguiri, Lero, Tri-K, Kalana and Yanfolila.

On a project scale, Sanankoro is characterised by the 2km wide Sanankoro Shear Zone, which can be traced over 30km from Kabaya South in the western Yanfolila Mine to north of the Niger River beyond Selin and onto Karan. Within the project area, each of the prospects are underpinned by a strong linear parallel, and where strong mineralisation is developed, a pronounced localised northeast-southwest focused zone of en-echelon veining and associated sulphide development.

There are five main areas which currently define the Sanankoro Gold project, which in order of significance are Selin, Zone A, Zone B, Zone B North, and Zone C.

Selin is hosted on the eastern margin of the Sanankoro Shear Zone in the north-eastern corner of the Sanankoro permit. The Selin deposit has a typical interference node control but with the additional positive impact of a strong, rheological diorite intrusive host. The gold geology at Selin is anchored along this linear, en-echelon or possibly folded, diorite igneous intrusive which cores the volcaniclastic thrust assemblage and focuses the gold deposition.

Recent core drilling into Selin has enlightened the genetic model for this resource deposit by discovering four to six multiple early/pre-D3 dykes of diorite intruding the 65-80° west dipping axial trace of a western hangingwall F3 anti-form on this major reactivated D2 east-verging thrust. The >100 m wide Selin Shear Zone may be a regional back-thrust and the dominant eastern margin of the regional west-verging Sanankoro Thrust. The largest diorite unit is demonstrably discordant and sits immediately west and adjacent to a major early ductile, 10-30 m wide footwall carbonaceous shear. Progressive deformation has folded, warped and possibly cross-faulted the diorite units prior to gold deposition. The early footwall shear fabrics are overprinted by later semi-brittle to brittle graphitic faults which locally convert all protolith to graphitic schist on sub-metre scale. The diorite units exhibit multi-phase veining interference and sulphide development. The dominant sulphide is pyrite with occasional arsenopyrite and a scattering of chalcopyrite. Alteration minerals are predominantly sericite, silica, fuchsite, ankerite, graphite and calcite.

Zone A shores up the southern limit of the 11.5km mineralised corridor, which forms the backbone to the Sanankoro Project. Zone A is the southern-most expression of the 010° trending central axis of the Sanankoro Shear Zone, which sits 900m west of the Selin Boundary Shear and hosts the 5.8km chain of open pit resources from Zone A through Zone B1, B2, B3 to Target 3. The deposits of this central trend verge westward mimicking the regional sense of thrusting.

Zone B is the strike extension of Zone A, located 800m to the north. The Sanankoro Main Trend runs for 6km from south end of Zone A to the north end of Target 3. Detailed sectional drilling is required along the length of this major generative gold system. The local structural facing and stratigraphy of Zone B is very similar to Zone A with the western footwall sequences hosting more crystalline volcanic tuffaceous units and the eastern, hangingwall assemblages being more basinal sediments. Zone B hosts an impressive scale of hydrothermal activity and the broad horizontal widths of mineralisation observed in the recent drilling bodes well for future discovery potential along the central and southern sections of the Sanankoro Main Shear Zone.

Zone C is located 650 m southwest of Zone A on the parallel, >7km long Sanankoro West Shear Zone (SWSZ) which can be traced along a chain of surface workings to the Excavator Prospect, 1.5km north-northwest of Target 3. The SWSZ is high in the priority list for drilling in the 2022 program and a number of SWSZ targets, beyond Zone C, will be tested for surface potential.

Zones A, B and C deposits are identical in style and typical of Siguiri Basin deposits, fold-thrust controlled within pelitic and psammitic sediments and very deeply weathered (>120 m from surface). There is a highly evolved weathering profile with a pronounced 8-10 m thick duricrust-laterite ferro-cap, grading downward into a well-developed mottled zone to 20-25 m depth and remains highly weathered until beyond 140 m vertically within the central mineralised fault zone. Zone B1 has extremely deep weathering with shallow oxide densities measured to depths of 190 m down-dip within the ore zone trough.

All the host oxide lithologies are weathered to kaolin with only highly corroded quartz vein material remaining in-situ to mark the main gold faults. Diamond core shows the host lithologies to be predominantly variably grained basinal pelites and sandstones with minor horizons of small quartz clast, matrix-supported greywacke inter-bedded within the sequence. A minor intercept of diorite has been identified but does not form an important control to the mineralisation currently drill tested at Zone A or C. The primary sulphide is pyrite disseminated around central vein networks and enveloped by a broader hydrothermal halo of silica flooding, sericite and ankerite.

Drillhole information

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

●  easting and northing of the drillhole collar

●  elevation or RL (Reduced Level - elevation above sea level in metres) of the drillhole collar

●  dip and azimuth of the hole

●  downhole length and interception depth

●  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.

Significant intercepts that form the basis of the MRE have been released in previous announcements (available on the Cora website) with appropriate tables incorporating Hole ID, Easting, Northing, From, Depth and Intercept Assay Data. Appropriate maps and plans accompany this MRE.

Previous drilling completed by Cora, Gold Fields and Randgold is documented herein.

A complete listing of all drillhole details is not necessary for this report which describes the Sanankoro Gold Project Mineral Resources and in the Competent Person's opinion the exclusion of this data does not detract from the understanding of this report.

The 2021 program twinned important historical Goldfields and early Cora, smaller diameter, air core and RC intercepts. Historical Energold DD NQ core holes exhibited sections of unacceptably poor recoveries, especially in the deeply oxidised deposits of Zone A and Zone B1, which were twinned using the deep RC rig.

The 2022 program focussed on infill drilling at Zone B North and Selin, and targeted Fode 1 and Target 6 as potential sites of interest.

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.

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.

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

All RC intersections are sampled and assayed on 1 m intervals but could be composited up to 4 m in areas interpreted to be barren.

DD core sampling can be 0.5-1.5 m in length depending on geological contacts.

Significant intercepts have previously been reported using a cut-off grade of 0.5 g/t, without top cuts.

Mineralised intervals were reported with a maximum of 3 m of consecutive internal dilution of less than 0.5 g/t Au. Mineralised intervals were reported on a length-weighted average basis.

No metal equivalents are reported.

Relationship between mineralisation widths and intercept lengths

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

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

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').

The orientation of the mineralised zone has been established and majority of the drilling was planned to intersect the mineralised structures orthogonally or as close as practicable.

Existing artisanal workings, buildings, sacred sites and drainage sometimes created obstacles which prevented perfect intersection and some holes were required to be drilled at less-than-ideal orientations.

For the bulk of drillholes, site preparations were carried out and50 m x 25 m drill spacing applied and acceptable intersection orientations were achieved.

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.

The appropriate plans and sections are included in this document.

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.

All grades, high and low, are reported accurately with "from" and "to" depths and "hole identification" shown.

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.

Detailed metallurgical test work has been carried out as part of a previous scoping study. Testwork shows that the ore is amenable to conventional crushing, grinding, gravity and carbon-in-leach processing. Oxide recoveries have been determined to be >95%.

1,068 detailed dry bulk density determinations were conducted on all 2021 drilled core.

589 detailed UCS point load determinations were conducted on all drilled fresh core.

Detailed geotechnical logging and analysis was conducted on all drill core.

Detailed regional exploration programs continue to generate new drill targets which will feed into potential Mineral Resource growth.

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).

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

Detailed ESIA studies commenced in Q2 2020 and stakeholder engagement meetings conducted throughout the period to date.

A program of detailed hydrology and civils geotechnical drilling is planned for water management, tailings storage facility and plant sites.

Detailed variability metallurgical testwork is planned at ALS Perth to support a feasibility study.

Detailed open pit and civils geotechnical studies are planned to support a feasibility study.

Detailed hydrology studies are planned to support a feasibility study.

Additional Mineral Resource, Ore Reserve and grade control pattern drilling is planned to update Ore Reserve designs prior to commencement of mining.

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 validation procedures used.

Cora has a dedicated, 30-year experienced Data Manager consultant (Mr Tim Kelemen) who devised and built the central Datashed™ database with standardised data collection templates, lookup tables and validation routines for all exploration logging, spatial and sampling data.

Data collection is updated nightly by the Senior Project Geologist and emailed as a quick-log to Tim in Brisbane for upload, validation and reporting. The quick-log Microsoft Excel file contains DRILL ACTUAL VS PLAN, COLLAR, DTH SURVEY, SAMPLING, GEOLOGY, VG LOGGING, WATER TABLE, INTERCEPTS and LAB SUBMISSION sheets.

Sample numbers are unique and pre-numbered bags are used.

Cora project geologists validate assays returned back to the drill logged geology in chips and core, previous section intercepts and on-going 3D interpretation within MICROMINE™.

The MRE data was further validated on import into MICROMINE™ mining software.

Cora employed routine 20% QAQC throughout all the 2021 and 2022 assaying stream, involving one standard, one blank, two duplicates and one triplicate which were inserted for every 25 samples submitted (5:25).

Detailed re-splits of important positive and negative intercepts were taken as directed by the Head of Exploration, re-assayed at various labs and cross-checked against original assays as selective QAQC.

A full record of access and database keystrokes is maintained within Datashed.

Tim Kelemen is the sole person with access to the Master DATASHED™ database, which consequently is held remotely in Brisbane and backed-up to the cloud nightly.

Site visits

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

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

The Competent Person for the MRE, Mr Anton Geldenhuys, visited the Sanankoro Project in October 2021. The visit included inspection of geology offices, RC Chip Library, DD Core Shed and Library, geotech rock lab and viewing sample/pulp stores, central bag farm, sampling sheds, drill sites, artisanal workings, and local surface geology.

DD coring was ongoing at Zone A and Zone B at the time of visit and the Competent Person observed geological/geotechnical logging and density determinations. A number of RC chip trays and DC holes were reviewed which form part of this MRE.

Geological interpretation

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

Nature of the data used and of any assumptions made.

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

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

The factors affecting continuity both of grade and geology.

The diorite intrusive at Selin plays a significant role in controlling the distribution and tenor of the mineralisation and consequently has been modelled as solid units within the enveloping gold mineralisation wireframe. The diorite intrusion precedes the gold mineralisation event and dips 70-85° to the west.

The main host protolith at Zones A, B, B North and C, and surrounding the diorite at Selin, are predominantly pelitic sediments and graphitic shears which similarly dip at moderate to high angles to the east.

Overprinting the strong linear north-south lithological architecture is a flat weathering stratigraphy which is characterised from surface with an iron indurated cap of laterite ± duricrust down to 12-17 m, with an underlying mottled zone of soft plastic clay and highly kaolinized laterite for a further 6-12 m. Below the mottled zone is the saprolite, a highly weathered discernible rock which is present, but down to highly variable depths, across the deposits, reaching depths of >170 m at Zone B. The saprolite can be observed to freshen into transition material relatively rapidly but extends to depths normally between 170 m and 200 m at Zone A and Zone B, in the highlands, before becoming true fresh rock.

At Selin, the weathering profile is suppressed, probably by the massive siliceous nature of the diorite, with the transition material occurring from 60 m in certain highly siliceous, veined mineralisation locations. The transition diorite mineralisation tends to maintain good CN recoveries.

Zone A and Zone B/North exhibit a very pronounced deep trough weathering profile whereas Zone C and Selin seem to host less pronounced weathering, likely due to host rock types and topographically low relief positions.

Mineralisation was modelled using a 0.2 g/t Au threshold value for all areas. The threshold is deemed to be an indicator of mineralised material.

Higher grade zones were investigated, but these proved to not be sufficiently continuous for modelling and estimation purposes.

The mineralisation model was guided by local dip and strike trends.

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.

Mineral Resource:

The Selin mineralisation model is 2.8km in length along strike, a maximum of 270 m in depth, and is anything from a few to 50 m wide. Selin is reported to a maximum depth of 220 m below surface.

The Zone A mineralisation model is 1.2km in length along strike, a maximum of 245m in depth, and is anything from a few to 50m wide. Zone A is reported to a maximum depth of 190m below surface.

The Zone B mineralisation model is 1.7km in length along strike, a maximum of 215m in depth, and is anything from a few to 50m wide. Zone B is reported to a maximum depth of 180m below surface.

The Zone C mineralisation model is 750m in length along strike, a maximum of 160m in depth, and is anything from a few to 50m wide. Zone C is reported to a maximum depth of 120m below surface.

The Zone B North mineralisation model is 1km in length along strike, a maximum of 130m in depth, and is anything from a few to 50m wide. Zone B North is reported to a maximum depth of 110m below surface.

Exploration Target:

Zone B mineralisation model is 1.7km along strike, a maximum of 215m in depth, and is anything from a few to 50m wide. Zone B is reported below the current RPEEE pit shell.

Selin mineralisation model is 2.8km along strike, a maximum of270m in depth, and is anything from a few to 50m wide. Selin is reported below the current RPEEE pit shell.

Zone A mineralisation model is 1.2km along strike, a maximum of 245m in depth, and is anything from a few to 50m wide. Zone A is reported below the current RPEEE pit shell.

Zone B North mineralisation model is 1km along strike, a maximum of 130m in depth, and is anything from a few to 50m wide. Zone B North is reported below the current RPEEE pit shell.

Zone A & C extension mineralisation model is 4km along strike (not continuous) and a maximum of 170m in depth and is anything from a few to 50m wide.

Selin Bokoro-East extension mineralisation model is 3.7km along strike (not continuous) and a maximum of 170m in depth and is anything from a few to 50m wide.

Bokoro-West mineralisation model is 0.7km along strike (not continuous) and a maximum of 130m in depth and is anything from a few to 50m wide.

Target 3 extension mineralisation model is 4.8km along strike (not continuous) and a maximum of 170m in depth and is anything from a few to 50m wide.

Target 5 and Target 6 mineralisation model is 3.7km along strike (not continuous) and a maximum of 120m in depth and is anything from a few to 50m wide.

Dako-Main mineralisation model is 2.0km along strike (not continuous) and a maximum of 140m in depth and is anything from a few to 50m wide.

Zone C mineralisation model is 750m in length along strike, a maximum of 160m in depth, and is anything from a few to 50m wide

Fode 1 mineralisation model is 0.7km in length along strike (not continuous) and a maximum of 130m in depth and is anything from a few to 50m wide.

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

The assumptions made regarding recovery of by-products.

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

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

Any assumptions behind modelling of selective mining units.

Any assumptions about correlation between variables.

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

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

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

Mineral Resource:

Samples were composited to 2m for all MRE processes.

Experimental semi-variograms were calculated for gold from composites in Zones A and B combined, and Selin. Zones B North and C were deemed to contain too few data for variography.

The modelled semi-variogram for Zone A + B combined was applied to Zones A, B, B North and C for grade estimation. The modelled semi-variogram for Selin was only used to estimate grade at Selin.

Estimation was carried out within the modelled 0.2 g/t Au mineralised volumes using ordinary kriging on 2m composites for gold. The entire volume was estimated such that estimates were extrapolated no more than 100m away from data. This was often downdip, however, reporting pit shells ensure that deep extrapolated grades were not included in the Mineral Resource.

Mineralisation boundaries were treated as hard contacts for estimation.

Ordinary kriging was optimised based on the kriging neighbourhood which ensured minimal negative kriging weights and representative local estimates.

Seequent Leapfrog Geo was used to model the mineralisation and Datamine RM was used to estimate grade and tabulate the Mineral Resource tonnages, grade, and content.

An Inverse distance weighting estimate was carried out as a check of the ordinary kriged estimates. These correlate well and the ordinary kriged estimate is deemed to be an acceptable representation of the in-situ gold grade.

No by-products or deleterious elements were considered in the MRE.

The parent cell size is 5m x 20m x 20m (XYZ). Collars were drilled at50m x 50m or 50m x 25m spacing. The block is deemed to be appropriate relative to the data configuration.

Search distance was roughly aligned to the variogram range (30m) for all zones.

Selective mining units were not considered in the estimation.

Composite gold grades were capped for estimation according to area, based on statistics and outliers. Selin composites were capped to 34 g/t Au, Zone A composites were capped to 20 g/t Au, Zone B composites were capped to 21 g/t Au, Zone B North composites were capped to 8.5 g/t Au and Zone C composites were capped to 6 g/t Au.

Gold grade estimates were validated by means of global statistics, swath plots and visual sectional checks of grade in the model vs grade of the composites.

Exploration Target:

Modelled in Leapfrog Geo using an indicator radial basis function interpolant from 2m composites. Due to the fairly consistent dip and strike in the Project area a simplified single planar structural trend was applied for modelling (dip azimuth 105°, dip 77°). A spheroidal interpolant was applied for modelling using a strength of 5:1 within the plane of mineralisation, relative to the strength perpendicular to the plane of mineralisation.

An iso value of 0.3 was applied for modelling the mineralisation contact. The mineralisation is generally consistent along strike and down dip and are similar in shape to the modelled areas of the MRE. The most significant geological risk identified is the uncertainty in the lateral depth extent and grade continuity of the gold mineralisation outside of the defined Indicated and Inferred Mineral Resource.

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 in the estimate are for dry tonnage with no factoring for moisture.

Cut-off parameters

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

The Mineral Resource is reported at a cut-off grade of 0.4 g/t Au, which is what was previously used to report the 2021 Mineral Resource.

The cut-off grade is in line with other similar reported styles of gold mineralisation.

The Exploration Target is reported at a cut-off grade of 0.4 g/t Au, the same as the Mineral Resource.

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.

The Mineral Resource is deemed to be amenable to open pit extraction.

Reasonable prospects for eventual economic extraction were determined using conceptual mining parameters and a long-term gold price of US$1,900/oz.

The parameters and long-term gold price were used in Whittle to determine a life of mine pit shell for reporting the Mineral Resource.

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.

Metallurgical testwork conducted upon Selin, Zones A and B gold ore composites - ALS Perth Report No. A21106, March 2021.

Results indicated +95% recoveries from grinding P80 passing 75-micron, gravity and direct CIL.

As significant program of metallurgical variability test work is ongoing at ALS Perth and will be incorporated into the forthcoming Definitive Feasibility Study.

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 greenfields 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.

Metallurgical testwork conducted upon Selin, Zones A and B Gold Ore Composites - ALS Perth Report No. A21106, March 2021. The acid mine drainage prediction analysis for all four composite samples indicated that none would be net acid-producers.

A significant program of AMS testwork is ongoing at ALS Perth and will be incorporated into the forthcoming Definitive Feasibility Study.

A full Definitive Feasibility Study-level ESIA study commenced in June 2020 by Digby Wells and will be incorporated into the forthcoming Definitive Feasibility Study.

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.

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.

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

Dry bulk density determinations were made using the water displacement method 6 as outlined in "AusIMM Monograph 30 - Measurement of Bulk Density for Resource Estimation" (Lipton and Horton).

Dried for 24 hours at 110°C, waxed and weighed using LTB 6002e 0.1 g electronic balance.

A total of 1,068 dry bulk density determinations were made on full PQ and HQ core samples.

Bulk density was analysed according to weathering domain by removing outlier values and determining mean values from representative data.

Mean values were applied to the weathering domains as follows: duricrust cap 2.23 t/m3; mottled zone 1.95 t/m3; oxide 1.86 t/m3; transition 2.58 t/m3 and fresh 2.74 t/m3.

The Exploration Target was split in oxide, transitional and fresh and the mean densities were applied as above.

Classification

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

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).

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

The Mineral Resource was classified into Indicated and Inferred categories as defined by The Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves ("the JORC Code").

Mineral Resource classification considered the quality and quantity of available data, geological continuity, grade continuity and confidence in the grade estimates.

Indicated Mineral Resources were classified from data that was deemed acceptable for Mineral Resource estimation and reporting, and where data were sufficient to model mineralisation and estimate grade with a reasonable level of confidence for Indicated Mineral Resources. Data was generally spaced at 35m x 35m in Zones A, B, B North and C, and at 40m x 40m at Selin. The mineralisation at Selin is deemed to be more continuous, hence the wider spacing allowed for Indicated. Indicated Mineral Resources have slope of regression values ≥0.75, demonstrating an acceptable level of confidence in the estimate.

Inferred Mineral Resources were classified beyond the 35m x 35m (Zones A, B, B North and C) and 40m x 40m (Selin) data spacing.

Mineral Resources were constrained by the reasonable prospects for eventual economic extraction pits, below which any mineralisation was not classified and therefore not reported.

Audits or reviews

The results of any audits or reviews of Mineral Resource estimates.

No Mineral Resource audit or review by the Competent Person for Mineral Resources, however, a site visit was carried out to review the data acquisition and processing practices.

Discussion of relative accuracy/ confidence

Where appropriate a statement of the relative accuracy and confidence level in the Mineral Resource estimate 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.

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.

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

The level of accuracy in the Mineral Resource is represented by the classification categories assigned to block model.

Indicated Mineral Resources can be considered as reasonable local estimates.

Inferred Mineral Resources are deemed to be global in nature.

No commercial production has taken place and therefore no production data is available for Mineral Resource reconciliation.