Cora Gold Limited (AIM:CORA) Second Drill Results from 2022 Drill Campaign

Cora Gold Limited, the West African focused gold company, is pleased to announce the second set of drill results from its recently completed 2022 drill programme at the Company’s Sanankoro Gold Project (‘Sanankoro’ or the ‘Project’) in southern Mali.

Highlights

● Reverse Circulation (‘RC’) drilling highlights from Zone B North:

o 17m @ 2.85 g/t gold (‘Au’) from 81m in hole SC0616

o 11m @ 1.99 g/t Au from 31m in hole SC0608

o 11m @ 1.35 g/t Au from 53m in hole SC0612

o 31m @ 0.97 g/t Au from 15m in hole SC0615

▪ Including 4m @ 2.18 g/t

o 11m @ 1.29 g/t Au from 10m in hole SC0618

● All Zone B North RC holes have now been released and RC assay results from Selin, Fode 1 and Target 6 will be released in the coming weeks

● Drill programme consisted of 11 aircore (‘AC’) shallow holes for 897m and 78 RC holes for a total of 6,992m (4,958m at Zone B North; 1,092m at Selin South, 504m at Fode 1 and 438m at Target 6)

● Drilling targeted both converting existing Inferred Mineral Resources to Indicated Mineral Resources, as well as identifying new discoveries at Sanankoro.

Bert Monro, Chief Executive Officer of Cora, commented, “The latest results from Zone B North once again show shallow oxide mineralisation of good widths and grade. 17m at 2.85 g/t Au is a very positive drill hole as we target upgrading the Zone B North deposit to Indicated Resources. We look forward to releasing the results from the final phase of the programme, which focussed on Selin and follow-up holes at the new discoveries at Fode 1 and Target 6, in the coming weeks.”

To view the RNS with illustrative diagrams and maps, please use the following link:
http://www.rns-pdf.londonstockexchange.com/rns/8314L_1-2022-5-17.pdf

Sanankoro Gold Project Map

Figure 1: Map showing the locations of the deposits and discoveries at the Sanankoro Gold Project

Background on the Geology

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 structural 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 30 km 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 NE-SW focused zone of en-echelon veining and associated sulphide development.

Selin Geology

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 deposit by discovering 4-6 multiple early/pre-D3 dykes of diorite intruding the 65-80° W dipping axial trace of a western hanging-wall F3 anti-form on this major reactivated D2 east-verging thrust. The >100m 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, 10-30m 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, Zone B and Zone C Geology

Zone A is the second major deposit at Sanankoro behind Selin and shores up the southern limit of the 11.5km mineralised corridor, which forms the backbone to the Sanankoro Project. Zone A is the southernmost expression of the 010o trending central axis of the Sanankoro Shear Zone, which is located 900m west of the Selin Boundary Shear and hosts the 5.8km chain of deposits from Zone A through Zone B to Zone B North. The deposits of this central trend verge westward mimicking the regional sense of thrusting.

Zone B is the third major deposit at Sanankoro behind Selin and Zone A. It is the strike extension of Zone A, located 800m to the north. The Sanankoro Main Trend strikes for 6km from the south end of Zone A to the north end of Zone B North. 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, hanging wall 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 (SMSZ).

Zone C is located 650m 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 NNW of Zone B North.

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 (>120m from surface). There is a highly evolved weathering profile with a pronounced 8-10m thick duricrust-laterite ferro-cap, grading downward into a well-developed mottled zone until 20-25m and remains highly weathered until beyond 130m vertically within the central mineralised fault zone. Below the saprolite lies a 35-40m thick transition zone ending on top of fresh rock at between 160 to 170m.

All of 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.

Intersections

The intersections have been calculated using a 0.4 g/t Au cut-off over a minimum 1m sample length. An allowance of 2m of internal material, below cut-off grade, is included where required. Lengths are apparent in nature and are therefore not true widths of the mineralisation.

All samples were sent for 2kg bottle roll analysis at ALS Laboratories with results supported by QAQC analysis.

Intersections are reported according to JORC 2012 guidelines.

Figure 2 : Plan view of Zone B North showing section lines (see Figure 3, Figure 4 and Figure 5)

The conceptual interpretation of mineralisation (Figure 3, Figure 4 and Figure 5) was made using a 0.2 g/t Au threshold i.e., the same threshold used for the Mineral Resource (November 2021). This interpretation is for illustrative purposes only and does not represent a volume or domain that will be used for Mineral Resource reporting purposes in future. The conceptual interpretation illustrates a thickening of the mineralisation in places, resulting in certain drill holes ending in mineralisation. This will be further investigated as more results become available from the 2022 drilling programme.

Figure 3 : Cross section 1 looking south at Zone B North showing new drill hole traces and samples relative to a conceptual interpretation of the mineralisation.

Figure 4: Cross section 2 looking south at Zone B North showing new drill hole traces and samples relative to a conceptual interpretation of the mineralisation.

Figure 5: Cross section 3 looking south at Zone B North showing new drill hole traces and samples relative to a conceptual interpretation of the mineralisation.

Table 1 : RC drill intercepts from the on-going 2022 drill programme.

Read More

Competent Person’s statement

The information in this release that relates to Exploration Results was reviewed by Mr Anton Geldenhuys, a Competent Person who is a Member of the South African Council for National Scientific Professions (SACNASP). Mr Geldenhuys (Principal Resource Consultant) is an independent consultant with CSA Global and has sufficient experience that is 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 Reporting of Exploration Results, Mineral Resources and Ore Reserves’. Mr Geldenhuys consents to the inclusion in this release of the Exploration Results in the form and context in which it appears. Mr Geldenhuys confirms that the information contained in the Appendix of this release that relates to the reporting of Exploration Results at Sanankoro is an accurate representation of the available data. In addition, Mr Anton Geldenhuys qualifies as a Competent Person in accordance with the guidance note for Mining, Oil & Gas Companies issued by the London Stock Exchange in respect of AIM Companies, which outlines standards of disclosure for mineral projects.

2022 Annual General Meeting (‘AGM’)

The Company always welcomes questions from its shareholders at its general meetings. In relation to the AGM to be held online at 12.00 p.m. (United Kingdom time) on 21 June 2022, the board of directors of the Company requests shareholders submit their questions in advance to ensure all questions can be compiled and answered either at the AGM or afterwards. Questions should be submitted by email to secretary@coragold.com no later than 12.00 p.m. (United Kingdom time) on 17 June 2022. For details on how attendees may join the AGM, see the announcement of 16 May 2022.

Market Abuse Regulation (‘MAR’) Disclosure

Certain information contained in this announcement would have been deemed inside information for the purposes of Article 7 of Regulation (EU) No 596/2014, which is part of UK law by virtue of the European Union (Withdrawal) Act 2018, until the release of this announcement.

**ENDS**

For further information, please visit http://www.coragold.com or contact:

Bert Monro

Craig Banfield

Cora Gold Limited

info@coragold.com


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