TIDMCORA
RNS Number : 7020K
Cora Gold Limited
09 May 2022
Cora Gold Limited / EPIC: CORA.L / Market: AIM / Sector:
Mining
9 May 2022
Cora Gold Limited ('Cora' or 'the Company')
First Drill Results from 2022 Drill Campaign & New Gold
Discoveries
Cora Gold Limited, the West African focused gold company, is
pleased to announce the first drill results from its 2022 drill
programme at the Company's Sanankoro Gold Project ('Sanankoro' or
the 'Project') in southern Mali.
-- Drill programme consisting of 11 aircore (AC) shallow holes
for 897m and 78 reverse circulation (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) now completed at Sanankoro.
-- Drilling targeted both converting existing Inferred Mineral
Resources to Indicated Mineral Resources, as well as identifying
new discoveries at Sanankoro.
-- RC drill highlights at Zone B North:
o 25m @ 2.38 g/t Au from 65m in hole SC0595
o 27m @ 1.40 g/t Au from 18m in hole SC0600
o 5m @ 4.64 g/t Au from 48m in hole SC0598
o 20m @ 1.09 g/t Au from 83m in hole SC0597
o 8m @ 2.47 g/t Au from 39m in hole SC0593
o 8m @ 1.88 g/t Au from 39m in hole SC0593
o 8m @ 1.74 g/t Au from 37m in hole SC0583
-- Two new discoveries - Fode 1 and Target 6 both in close
proximity to existing Mineral Resources
-- AC drill highlights:
o 2m @ 3.56 g/t Au from 41m in hole SC0572 at Fode 1
o 6m @ 0.65 g/t Au from 66m, including 2m @ 1.62 g/t Au in hole
SC0573 at Fode 1
o 3m @ 1.24 g/t Au from 7m in hole SC0579 at Target 6
o Awaiting results from RC follow up drill holes at these
discoveries
-- Drill results consist of all the AC holes and the first 28 RC
holes completed at Zone B North. Drill results for the later RC
holes are expected imminently.
Bert Monro, Chief Executive Officer of Cora, commented, "Our
2022 drill programme has a dual focus; to both increase the
Indicated Mineral Resources at Sanankoro through conversion of
existing Inferred material and to target new discoveries to add to
the project growth potential in the future. The recent
identification of two new gold discoveries, Fode 1 and Target 6, is
an exciting new development and we look forward to getting the RC
drill results that followed up the initial shallow AC holes.
"The first holes of the RC programme have delivered a number of
shallow oxide intercepts, including 25m @ 2.38 g/t Au, which
continues to give us early encouragement from the first holes of
the programme."
To view the RNS with illustrative diagrams and maps, please use
the following link:
http://www.rns-pdf.londonstockexchange.com/rns/7020K_1-2022-5-8.pdf
New Discoveries
Figure 1: Map showing the locations of the two new drilled gold
discoveries; Fode 1 and Target 6 at Sanankoro.
Figure 2: Fode 1 target showing the AC collars relative to the
ground geophysics IP anomaly. The red dots show collars with gold
intercepts in Table 1.
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 2 km 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 65-80deg 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 11.5 km mineralised corridor,
which forms the backbone to the Sanankoro Project. Zone A is the
southernmost expression of the 010(o) trending central axis of the
Sanankoro Shear Zone, which is located 900m west of the Selin
Boundary Shear and hosts the 5.8 km 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 6 km 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, +7
km long Sanankoro West Shear Zone (SWSZ) which can be traced along
a chain of surface workings to the Excavator Prospect, 1.5 km 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 in 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 0.1 g/t Au
cut-off over a minimum 1m sample length. An allowance of 3 m 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 (see Figure 4 and Figure 5).
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 3: Plan view of Zone B North and Fode 1 showing section
lines (see Figure 4 and Figure 5)
The conceptual interpretation of mineralisation (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 drillholes ending in mineralisation. This will be
further investigated as more result become available from the 2022
drilling programme.
Figure 4: 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 5: Cross section 2 looking south at Zone B North showing
new drill hole traces and samples relative to a conceptual
interpretation of the mineralisation.
Table 1 : AC and RC drill intercepts from the on-going 2022
drill programme.
Hole Easting Northing From To Width Au Intercept Including Drill Prospect
(g/t) type
3 m @ 0.52
SC0569 558022 1300947 57 60 3 0.52 g/t AC FODE_1
3 m @ 0.53
SC0569 558022 1300947 69 72 3 0.53 g/t AC FODE_1
SC0570 558021 1301100 0 0 0 No intersection AC FODE_1
5 m @ 0.20
SC0571 557976 1301101 75 80 5 0.20 g/t AC FODE_1
2 m @ 3.89
SC0572 557881 1301099 41 43 2 3.89 g/t AC FODE_1
6 m @ 0.74 2 m @ 1.85
SC0573 557927 1300950 66 72 6 0.74 g/t g/t AC FODE_1
SC0574 557920 1301046 No intersection AC FODE_1
SC0575 557965 1301050 No intersection AC FODE_1
3 m @ 3.29
SC0576 557922 1300647 9 12 3 3.29 g/t AC FODE_1
3 m @ 0.27
SC0576 557922 1300647 21 24 3 0.27 g/t AC FODE_1
1 m @ 0.20
SC0576 557922 1300647 46 47 1 0.20 g/t AC FODE_1
2 m @ 0.46
SC0577 557916 1300702 27 29 2 0.46 g/t AC FODE_1
2 m @ 1.39
SC0577 557916 1300702 32 34 2 1.39 g/t AC FODE_1
3 m @ 0.13
SC0578 558100 1294553 51 54 3 0.13 g/t AC Target6
3 m @ 0.18
SC0578 558100 1294553 66 69 3 0.18 g/t AC Target6
3 m @ 0.12
SC0579 558041 1294547 0 3 3 0.12 g/t AC Target6
3 m @ 1.34 2 m @ 1.94
SC0579 558041 1294547 7 10 3 1.34 g/t g/t AC Target6
1 m @ 0.56
SC0579 558041 1294547 13 14 1 0.56 g/t AC Target6
2 m @ 0.37
SC0579 558041 1294547 45 47 2 0.37 g/t AC Target6
3 m @ 0.16
SC0579 558041 1294547 57 60 3 0.16 g/t AC Target6
3 m @ 0.18
SC0579 558041 1294547 66 69 3 0.18 g/t AC Target6
7 m @ 1.22 Zone B
SC0580 558540 1299834 33 40 7 1.22 g/t RC North
1 m @ 0.45 Zone B
SC0581 558565 1299832 34 35 1 0.45 g/t RC North
6 m @ 0.29 Zone B
SC0581 558565 1299832 38 44 6 0.29 g/t RC North
2 m @ 0.83 Zone B
SC0581 558565 1299832 62 64 2 0.83 g/t RC North
13 m @ 0.24 Zone B
SC0581 558565 1299832 67 80 13 0.24 g/t RC North
Zone B
SC0582 558588 1299832 No intersection RC North
4 m @ 1.65 2 m @ 3.04 Zone B
SC0583 558534 1299777 18 22 4 1.65 g/t g/t RC North
2 m @ 1.81 1 m @ 2.79 Zone B
SC0583 558534 1299777 25 27 2 1.81 g/t g/t RC North
1 m @ 0.21 Zone B
SC0583 558534 1299777 33 34 1 0.21 g/t RC North
7 m @ 2.22 2 m @ 5.15 Zone B
SC0583 558534 1299777 37 44 7 2.22 g/t g/t RC North
2 m @ 0.21 Zone B
SC0584 558572 1299780 70 72 2 0.21 g/t RC North
6 m @ 0.52 Zone B
SC0584 558572 1299780 82 88 6 0.52 g/t RC North
6 m @ 0.54 Zone B
SC0585 558533 1299745 22 28 6 0.54 g/t RC North
11 m @ 1.24 3 m @ 3.30 Zone B
SC0585 558533 1299745 42 53 11 1.24 g/t g/t RC North
1 m @ 2.06 Zone B
SC0586 558563 1299746 15 16 1 2.06 g/t RC North
15 m @ 0.46 1 m @ 1.61 Zone B
SC0586 558563 1299746 64 79 15 0.46 g/t g/t RC North
1 m @ 0.45 Zone B
SC0586 558563 1299746 84 85 1 0.45 g/t RC North
26 m @ 1.06 10 m @ 1.53 Zone B
SC0587 558533 1299717 27 53 26 1.06 g/t g/t RC North
1 m @ 0.22 Zone B
SC0587 558533 1299717 55 56 1 0.22 g/t RC North
4 m @ 0.62 Zone B
SC0587 558533 1299717 57 61 4 0.62 g/t RC North
3 m @ 0.70 Zone B
SC0588 558551 1299714 58 61 3 0.70 g/t RC North
9 m @ 0.47 Zone B
SC0589 558534 1299670 53 62 9 0.47 g/t RC North
Zone B
SC0590 558052 1294546 No intersection North
10 m @ 0.43 Zone B
SC0591 558524 1299640 47 57 10 0.43 g/t RC North
10 m @ 0.62 1 m @ 1.77 Zone B
SC0592 558550 1299865 36 46 10 0.62 g/t g/t RC North
8 m @ 2.47 3 m @ 5.60 Zone B
SC0593 558577 1299864 39 47 8 2.47 g/t g/t RC North
1 m @ 0.19 Zone B
SC0593 558577 1299864 67 68 1 0.19 g/t RC North
5 m @ 0.33 Zone B
SC0593 558577 1299864 72 77 5 0.33 g/t RC North
2 m @ 0.79 Zone B
SC0593 558577 1299864 80 82 2 0.79 g/t RC North
10 m @ 1.07 2 m @ 3.76 Zone B
SC0593 558577 1299864 84 94 10 1.07 g/t g/t RC North
Zone B
SC0594 558600 1299865 No intersection North
8 m @ 1.14 2 m @ 2.81 Zone B
SC0595 558560 1299912 45 53 8 1.14 g/t g/t RC North
2 m @ 21.71
25 m @ 2.38 g/t; 2m @ Zone B
SC0595 558560 1299912 65 90 25 2.38 g/t 2.25 g/t RC North
1 m @ 0.41 Zone B
SC0595 558560 1299912 96 97 1 0.41 g/t RC North
1 m @ 0.18 Zone B
SC0595 558560 1299912 104 105 1 0.18 g/t RC North
Zone B
SC0596 558615 1299915 No intersection North
4 m @ 0.39 Zone B
SC0597 558669 1299950 11 15 4 0.39 g/t RC North
20 m @ 1.09 5 m @ 3.44 Zone B
SC0597 558669 1299950 83 103 20 1.09 g/t g/t RC North
2 m @ 0.81 Zone B
SC0598 558595 1299950 13 15 2 0.81 g/t RC North
5 m @ 4.64 2 m @ 10.75 Zone B
SC0598 558595 1299950 48 53 5 4.64 g/t g/t RC North
1 m @ 0.71 Zone B
SC0598 558595 1299950 76 77 1 0.71 g/t RC North
11 m @ 0.4 Zone B
SC0598 558595 1299950 100 111 11 0.40 g/t RC North
1 m @ 0.23 Zone B
SC0599 558630 1299950 5 6 1 0.23 g/t RC North
10 m @ 2.43
27 m @ 1.4 g/t; 4 m Zone B
SC0600 558590 1299995 18 45 27 1.40 g/t @ 2.17 g/t RC North
1 m @ 0.20 Zone B
SC0601 558614 1299995 5 6 1 0.20 g/t RC North
1 m @ 0.18 Zone B
SC0601 558614 1299995 16 17 1 0.18 g/t RC North
17 m @ 0.62 3 m @ 1.59 Zone B
SC0601 558614 1299995 61 78 17 0.62 g/t g/t RC North
1 m @ 5.81 Zone B
SC0601 558614 1299995 89 90 1 5.81 g/t RC North
8 m @ 0.52 Zone B
SC0602 558589 1300031 9 17 8 0.52 g/t RC North
17 m @ 0.32 Zone B
SC0602 558589 1300031 26 43 17 0.32 g/t RC North
1 m @ 0.58 Zone B
SC0602 558589 1300031 50 51 1 0.58 g/t RC North
1 m @ 6.04 Zone B
SC0603 558593 1300081 2 3 1 6.04 g/t RC North
10 m @ 0.67 2 m @ 1.61 Zone B
SC0603 558593 1300081 11 21 10 0.67 g/t g/t RC North
1 m @ 0.18 Zone B
SC0603 558593 1300081 24 25 1 0.18 g/t RC North
10 m @ 0.72 3 m @ 1.66 Zone B
SC0603 558593 1300081 41 51 10 0.72 g/t g/t RC North
1 m @ 0.17 2 m @ 1.97 Zone B
SC0604 558615 1300080 2 3 1 0.17 g/t g/t RC North
8 m @ 0.58 Zone B
SC0604 558615 1300080 36 44 8 0.58 g/t RC North
3 m @ 0.23 Zone B
SC0604 558615 1300080 63 66 3 0.23 g/t RC North
8 m @ 1.59 4 m @ 2.76 Zone B
SC0605 558595 1300117 9 17 8 1.59 g/t g/t RC North
16 m @ 0.40 1 m @ 1.56 Zone B
SC0605 558595 1300117 27 43 16 0.40 g/t g/t RC North
1 m @ 0.20 Zone B
SC0605 558595 1300117 47 48 1 0.20 g/t RC North
7 m @ 1.58 1 m @ 9.12 Zone B
SC0605 558595 1300117 55 62 7 1.58 g/t g/t RC North
1 m @ 0.19 Zone B
SC0606 558615 1300117 19 20 1 0.19 g/t RC North
2 m @ 0.45 Zone B
SC0606 558615 1300117 28 30 2 0.45 g/t RC North
8 m @ 0.37 Zone B
SC0606 558615 1300117 34 42 8 0.37 g/t RC North
1 m @ 0.21 Zone B
SC0606 558615 1300117 49 50 1 0.21 g/t RC North
13 m @ 0.63 1 m @ 3.85 Zone B
SC0606 558615 1300117 54 67 13 0.63 g/t g/t RC North
14 m @ 2.83 11 m @ 3.50 Zone B
SC0607 558610 1300150 15 29 14 2.83 g/t g/t RC North
3 m @ 0.21 Zone B
SC0607 558610 1300150 46 49 3 0.21 g/t RC North
13 m @ 0.34 Zone B
SC0607 558610 1300150 57 70 13 0.34 g/t RC North
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.
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.
**S**
For further information, please visit http://www.coragold.com or
contact:
Bert Monro Cora Gold Limited info@coragold.com
Craig Banfield
Christopher Raggett / Charlie finnCap Ltd +44 (0) 20 7220
Beeson (Nomad & Joint Broker) 0500
Andy Thacker Turner Pope Investments +44 (0) 20 3657
James Pope (Joint Broker) 0050
Susie Geliher / Selina Lovell St Brides Partners pr@coragold.com
(Financial PR)
Notes
Cora is an emerging West African gold developer with three
principal de-risked project areas within two known gold belts in
Mali and Senegal covering c.1,000 sq. km. Led by a team with a
proven track record in making multi-million-ounce gold discoveries
that have been developed into operating mines, its primary focus is
on developing the Sanankoro Gold Project in the Yanfolila Gold
Belt, Southern Mali, where Cora hopes to commence construction of
an open pit oxide focussed gold mine in 2022. An updated mineral
resource estimate on the Project was published in November 2021
which increased the Resources by over 200% (from the 2019 Maiden
resource) to 809,300oz Au. A Definitive Feasibility Study is
expected to be completed in H1 2022.
Appendix - JORC Code (2012) Edition, Table 1
Section 1: Sampling Techniques and Data
(Criteria in this section apply to all succeeding sections)
Criteria JORC Code explanation Commentary
Sampling Nature and quality This 2021/2022 phase of drilling is
techniques of sampling (e.g. cut composed of 6,993 m of RC and 897
channels, random chips, m of aircore (AC) drilling.
or specific specialised RC was ubiquitously sampled on 1 m
industry standard intervals. Each rod string is 6 m
measurement in length and is checked and marked
tools appropriate to with grease every 1 m to allow personnel
the minerals under to observe sampling and drill progress.
investigation, such The driller will sound a horn at the
as downhole gamma end of each 1 m interval, warning
sondes, the samplers to switch bags at the
or handheld XRF cyclone.
instruments, All industry standard RC sample quality
etc.). These examples procedures were applied, and each
should not be taken shift a geologist was present to ensure
as limiting the broad sample quality was maintained, holes
meaning of sampling. were not stopped in mineralisation
Include reference and activity reporting monitored cost
to measures taken to control. No detailed logging or sampling
ensure sample was conducted at the rigs.
representivity All bulk 1 m samples were transported
and the appropriate immediately upon hole completion to
calibration of any a central bag farm next to the Sanankoro
measurement tools or camp. No samples were left in the
systems used. field. All samples drilled were shipped
Aspects of the to the bag farm for splitting and
determination logging under controlled and secured
of mineralisation that conditions.
are Material to the The 1 m bulk samples are riffle split
Public Report. down to 5-6 kg using a three-tier
In cases where 75:25 riffle splitter and a duplicate
'industry pair of 2-3 kg samples are then generated
standard' work has using a two-tier 50:50 riffle splitter.
been done this would One sample is sent to the lab and
be relatively simple the duplicate is stored for any future
(e.g. 'reverse re-assay or reference.
circulation All RC holes are photographed on chip
drilling was used to tables and chip trayed after sampling
obtain 1 m samples and logging.
from which 3 kg was All RC holes are geologically logged
pulverised to produce and panned for visible gold on
a 30 g charge for fire 1 m intervals concurrently with sampling.
assay'). In other The logging and panning results dictate
cases, whether the logging or senior geologist
more explanation may will instruct compositing in less
be required, such as favourable intersections of a hole.
where there is coarse Composites of 4 m are possible in
gold that has inherent barren intersections.
sampling problems. The RC samples were sent to an accredited
Unusual commodities laboratory where they were pulverised
or mineralisation types to 85% passing 75 micron in a Labtechnics
(e.g. submarine LM2 puck pulveriser and sub-sampled
nodules) to provide 2 kg for CN bottle roll
may warrant disclosure and/or a 50 g aliquot for fire assay.
of detailed Bottle roll is the preferred assaying
information. method for oxide materials and fire
assay for fresh or sulphide-rich material.
AC was sampled and analysed as per
the RC procedure.
Drilling Drill type (e.g. core, RC was drilled using a 5(3/8) " face-sampling
techniques reverse circulation, hammer.
open-hole hammer, All drilling details and dates are
rotary recorded on hole logs and are stored
air blast, auger, in the COLLAR file in DATASHED(TM).
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 Method of recording RC was drilled using a 5(3/8) " face-sampling
recovery and assessing core hammer leading a 4(1/2) " standard
and chip sample rod string. Auxiliary booster-compressor
recoveries air packs were used on deeper holes,
and results assessed. normally >110 m, to ensure dry sample
Measures taken to quality and recovery.
maximise sample The RC drilling was sampled on a standard
recovery 1 m interval and recoveries assessed
and ensure quantitively by weighing each sampled
representative metre. A total of 6,698 RC samples
nature of the samples. and 844 AC weights were recorded during
Whether a relationship this drilling campaign in 2021/2022.
exists between sample The practice of weighing drill chip
recovery and grade samples immediately from recovery
and whether sample at the rig is Cora Gold Limited (Cora
bias may have occurred Gold) standard practice for all AC
due to preferential and RC drilling.
loss/gain of Sample quality and recovery are monitored
fine/coarse at the rig during drilling shift both
material. 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.
RC recoveries are logged and recorded
in the database. Overall recoveries
are >70% for the RC; there are no
significant sample recovery issues.
A geologist is always present at the
rig to monitor and record sample quality.
Logging Whether core and chip All RC holes are logged, panned and
samples have been sampled on a standard 1 m resolution.
geologically Every 1 m drilled is logged and panned
and geotechnically before being sampled.
logged to a level of 4 m compositing may be instructed
detail to support in barren sections of drilled hole
appropriate based on the results of the detailed
Mineral Resource logging.
estimation, All RC holes are photographed on chip
mining studies and tables and chip trayed after sampling
metallurgical studies. and logging.
Whether logging is
qualitative or
quantitative
in nature. Core (or
costean, channel, etc.)
photography.
The total length and
percentage of the
relevant
intersections logged.
Subsampling If core, whether cut All AC and RC chip samples were weighed
techniques or sawn and whether and riffle split to 2-3 kg for submission
and sample quarter, half or all to the lab. All AC and RC holes are
preparation core taken. sampled in bulk, logged and panned
If non-core, whether on a standard 1 m interval. Compositing
riffled, tube sampled, to 4 m may occur in barren geology.
rotary split, etc. A standard 5:25 sample QAQC was used
and whether sampled throughout the 2021/2022 programme,
wet or dry. composed of one standard, one blank,
For all sample types, two duplicates, and one triplicate.
the nature, quality Assay batches had a routine 20% QAQC
and appropriateness component.
of the sample The database manager monitors all
preparation sampling and QAQC vetting of the assay
technique. batches.
Quality control Field duplicates assist in determining
procedures the representivity of subsamples.
adopted for all QC category ratiosQC category DH sample QC sample Ratio
subsampling count count of QC samples
stages to maximise to DH samples
representivity of Field duplicate 5,101 471 1:11
samples. Triplicate
Measures taken to (Second
ensure that the Field duplicate) 5,101 213 1:24
sampling
is representative of Subsamples are deemed appropriate
the in-situ material for the reporting of Exploration Results.
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.
Quality The nature, quality Sample preparation involved oven drying,
of assay and appropriateness jaw crushing core P70 passing 2 mm,
data and of the assaying and followed by total pulverisation through
laboratory laboratory procedures an LM2 puck pulveriser to a nominal
tests used and whether the 85% passing 75 microns.
technique is considered Historically it has been proven that
partial or total. the nuggety, highly weathered nature
For geophysical tools, of the Sanankoro oxide mineralisation
spectrometers, handheld is best head assayed by 2 kg bottle
XRF instruments, etc, roll/atomic absorption spectrometry
the parameters used (AAS) with a 50 g fire assay/AAS on
in determining the the bottle roll tail residue on all
analysis including samples with Au values greater than
instrument make and 0.1 g/t Au. The bulk of the assay
model, reading times, database is completed by this method.
calibrations factors A total of 29,899 bottle roll (Leachwell)
applied and their assays were reported with 7,561 fire
derivation, assay/AAS tails.
etc. A standard 5:25 sample QAQC was used
Nature of quality throughout the programme, composed
control procedures of one standard, one blank, two duplicates,
adopted (e.g. and one triplicate. The assay batches
standards, had a routine 20% QAQC component.
blanks, duplicates, Standard type ratiosStandard DH sample Standard Standard Ratio
external laboratory type count type sample of QC standard
checks) and whether count count to DH samples
acceptable levels of BLANK 5,101 1 285 1:18
accuracy (i.e. lack CRM 5,101 5 241 1:21
of bias) and precision
have been established. Certified reference material (CRM)
standards were sourced from accredited
suppliers Rocklabs.Standard Expected Expected No. Supplier
code value standard of samples
deviation
OXG140 1.019 0.022 43 Rocklabs
OXK160 3.674 0.078 42 Rocklabs
SJ111 2.812 0.068 26 Rocklabs
SH98 1.400 0.028 26 Rocklabs
OXL159 5.349 0.139 74 Rocklabs
Following review of the QAQC, the
data are deemed appropriate for the
reporting of Exploration Results.
Verification The verification of The Competent Person has visually
of sampling significant verified some significant RC intersections
and assaying intersections during the site visit related to the
by either independent Mineral Resource in 2021.
or alternative company Geology and sampling data were logged
personnel. into Microsoft Excel format templates
The use of twinned and sent via email to the database
holes. manager. Files were imported into
Documentation of Datashed via configured importers
primary and passed through stringent validation.
data, data entry Validation included:
procedures, -- Logging codes checked against approved
data verification, code lists
data storage (physical -- Interval overlaps and gaps
and electronic) -- Records beyond end-of-hole.
protocols. All digital files received were archived
Discuss any adjustment on the workstation hosting the database.
to assay data. 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.
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 this
estimate.
Location Accuracy and quality Grid System: WGS84 UTM zone 29N (EPSG:
of data of surveys used to 32629)
points locate drillholes All surface survey features were surveyed
(collar with a LEICA GS18-T RTK differential
and downhole surveys), global positioning system (GPS) to
trenches, mine workings within a proven accuracy of 30 cm;
and other locations Cora conducted the differential GPS
used in Mineral work.
Resource A large number of well distributed
estimation. ground control points and features
Specification of the were used for the TERRABOTICS satellite
grid system used. survey. All points were set-out or
Quality and adequacy picked-up using CG-LEICA.
of topographic control. TERRABOTICS UK produced a site specific
139 km(2) digital terrain model (DTM)
with 0.3 m RL accuracy using tasked
MAXAR orthorectified WV3 imagery flown
in November-December 2020. The DTM
was provided in February 2021 and
utilised throughout the latest drill
program from March to August 2021.
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 139
km(2) area of interest accurately.
The WV3 imagery maps the full cadastral
and natural features across the project
area.
The 2022 drilling utilised a WELLFORCE
CHAMP north-seeking gyro throughout
and every drilled RC hole has a detailed
gyro DTH survey file. Historically,
DTH surveys were conducted, used a
REFLEX EZ-TRAC.
Data spacing Data spacing for The nominal drillhole collar spacing
and distribution reporting is 50 m x 25 m and 50 m x 50 m.
of Exploration Results. Due to the orientation of drill traces
Whether the data on section, data between drillholes
spacing can be spaced as close as 10 m in
and distribution is places.
sufficient to establish At this stage, no assessment of geological
the degree of and grade continuity has been conducted.
geological
and grade continuity
appropriate for the
Mineral Resource and
Ore Reserve estimation
procedure(s) and
classifications
applied.
Whether sample
compositing
has been applied.
Orientation Whether the orientation The bulk of the drilling is orientated
of data of sampling achieves 090deg or 270deg orthogonal to the
in relation unbiased sampling of strike of the mineralised domains.
to geological possible structures Structural logging based on oriented
structure and the extent to which core indicates that the main mineralisation
this is known, controls are +/-20deg from 000 north
considering and largely perpendicular to drill
the deposit type. direction.
If the relationship No orientation-based sampling bias
between the drilling has been identified in the dataset.
orientation and the
orientation of key
mineralised structures
is considered to have
introduced a sampling
bias, this should be
assessed and reported
if material.
Sample The measures taken The full chain of custody is managed
security to ensure sample by Cora. Samples collected daily from
security. 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 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 The results of any Cora's Head of Exploration at the
or reviews audits or reviews of time visited each of the labs in November
sampling techniques and December 2020 before signing contracts.
and data. No issues were identified during the
visit.
Section 2: Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this
section)
Criteria JORC Code explanation Commentary
Mineral Type, reference name/number, The Sanankoro Gold Project (area 341.87
tenement location and ownership km(2) ) is located in the Yanfolila
and land including agreements Gold Belt of southern Mali. The Sanankoro
tenure status or material issues Gold Project comprises five contiguous
with third parties gold exploration permits, being Bokoro
such as joint ventures, II (area 63.1 km(2) ; expiry date
partnerships, overriding 25 August 2023), Bokoro-Est (area
royalties, native title 100 km(2) ; expiry date 18 September
interests, historical 2028), Dako II (area 44.66 km(2) ;
sites, wilderness or expiry date 31 December 2027), Kodiou
national park and environmental (area 50 km(2) ; expiry date 15 May
settings. 2023), and Sanankoro II (see below).
The security of the The Definitive Feasibility Study is
tenure held at the focused on Mineral Resources within
time of reporting along the Sanankoro II gold exploration
with any known impediments permit.
to obtaining a license In accordance with the 2019 Mining
to operate in the area. Code of the Republic of Mali, the
84.11 km(2) Sanankoro II gold exploration
permit was awarded to Cora Resources
Mali SARL on 2 March 2021 (Arrêté
no. 2021-0590-MMEE/SG). Cora Resources
Mali SARL is registered in the Republic
of Mali. The duration of the permit
is three years, renewable twice at
the holder's request, the duration
of each renewal period is extended
to three years - as such, the full-term
expiry date of the Sanankoro gold
exploration permit is 2 March 2030.
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 Ressources SARL.
This permit expired on 1 February
2020, having been initially awarded
on 1 February 2013.
Exploration Acknowledgment and Exploration activities on the original
done by appraisal of exploration Sanankoro permit by previous workers
other parties by other parties. 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 to
50 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. Chris
Barrett SRK UK - Principal Exploration
Geologist visited Sanankoro from 27
to 30 March 2017 to bless the deal.
SRK UK, however, never returned to
site to do any Competent Person due
diligence for the 2019 MRE, due to
security concerns.
Geology Deposit type, geological Sanankoro is located on the leading
setting, and style western edge of the Yanfolila-Kalana
of mineralisation. 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 2 km 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 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 65-80deg
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 11.5 km mineralised corridor,
which forms the backbone to the Sanankoro
Project. Zone A is the southern-most
expression of the 010deg trending
central axis of the Sanankoro Shear
Zone, which sits 900 m west of the
Selin Boundary Shear and hosts the
5.8 km 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 800 m to the north.
The Sanankoro Main Trend runs for
6 km 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, >7 km long
Sanankoro West Shear Zone (SWSZ) which
can be traced along a chain of surface
workings to the Excavator Prospect,
1.5 km 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 A summary of all information Significant intercepts that form the
information material to the understanding basis of the MRE have been released
of the exploration to the AIM in previous announcements
results including a (available on the Cora website) with
tabulation of the following appropriate tables incorporating Hole,
information for all Easting, Northing, From, Depth and
Material drillholes: Intercept Assay Data.
-- easting and northing Appropriate maps and plans accompany
of the drillhole collar these Exploration Results.
-- elevation or RL Previous drilling completed by Cora,
(Reduced Level - elevation Gold Fields and Randgold is documented
above sea level in herein and in the publicly available
metres) of the drillhole report "Sanankoro Gold Project, Mineral
collar Resource Estimate" prepared by CSA
-- dip and azimuth Global UK and dated January 2022.
of the hole A complete listing of all drillhole
-- downhole length details is not necessary for this
and interception depth release which describes the intersections
-- hole length. of the latest drill programme. In
If the exclusion of the Competent Person's opinion the
this information is exclusion of this data does not detract
justified on the basis from the understanding of the Exploration
that the information results contained herein.
is not Material and The 2021 programme twinned important
this exclusion does historical Goldfields and early Cora
not detract from the Gold, smaller diameter, AC and RC
understanding of the intercepts. Historical Energold DD
report, the Competent NQ core holes exhibited sections of
Person should clearly unacceptably poor recoveries, especially
explain why this is in the deeply oxidised deposits of
the case. Zone A and Zone B1, which were twinned
using the deep RC rig.
Data aggregation In reporting Exploration All RC intersections are sampled and
methods Results, weighting assayed on 1 m intervals but could
averaging techniques, be composited up to 4 m in areas interpreted
maximum and/or minimum to be barren.
grade truncations (e.g. Significant intercepts have previously
cutting of high grades) been reported using a cut-off grade
and cut-off grades of 0.5 g/t, without top cuts.
are usually Material Mineralised intervals are reported
and should be stated. with a maximum of 3 m of consecutive
Where aggregate intercepts internal dilution of less than 0.5g/t
incorporate short lengths Au. Mineralised intervals are reported
of high grade results on a length-weighted average basis.
and longer lengths No metal equivalents are reported.
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.
Relationship These relationships The orientation of the mineralised
between are particularly important zone has been established and majority
mineralisation in the reporting of of the drilling was planned to intersect
widths and Exploration Results. the mineralised structures orthogonally
intercept If the geometry of or as close as practicable.
lengths the mineralisation Existing artisanal workings, buildings,
with respect to the sacred sites and drainage sometimes
drillhole angle is created obstacles which prevented
known, its nature should perfect intersection and some holes
be reported. were required to be drilled at less-than-ideal
If it is not known orientations.
and only the downhole For the bulk of drillholes, site preparations
lengths are reported, were carried out and
there should be a clear 35 m x 25 m drill spacing applied
statement to this effect and acceptable intersection orientations
(e.g. 'downhole length, were achieved.
true width not known').
Diagrams Appropriate maps and The appropriate plans and sections
sections (with scales) are included in this document.
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.
Balanced Where comprehensive All grades, high and low, are reported
reporting reporting of all Exploration accurately with "from" and "to" depths
Results is not practicable, and "hole identification" shown.
representative reporting
of both low and high
grades and/or widths
should be practiced
to avoid misleading
reporting of Exploration
Results.
Other substantive Other exploration Detailed metallurgical test work has
exploration data, if meaningful been carried out as part of a previous
data and material, should scoping study. Testwork shows that
be reported including the material is amenable to conventional
(but not limited to): crushing, grinding, gravity and carbon-in-leach
geological observations; processing. Oxide recoveries have
geophysical survey been determined to be >95%. An updated
results; geochemical metallurgical variability testwork
survey results; bulk program is ongoing at ALS Perth.
samples - size and 1.068 detailed dry bulk density determinations
method of treatment; were conducted on all 2021 drilled
metallurgical test core. 589 detailed UCS point load
results; bulk density, determinations were conducted on all
groundwater, geotechnical drilled fresh core. Detailed geotechnical
and rock characteristics; logging and analysis was conducted
potential deleterious on all drill core.
or contaminating substances. Detailed regional exploration programs
continue to generate new drill targets
which will feed into potential Mineral
Resource growth.
Further The nature and scale Detailed ESIA studies commenced in
work of planned further Q2 2020 and stakeholder engagement
work (e.g. tests for meetings conducted throughout the
lateral extensions period to date.
or depth extensions A program of detailed hydrology and
or large-scale step-out civils geotechnical drilling is planned
drilling). for water management, tailings storage
Diagrams clearly highlighting facility and plant sites.
the areas of possible Detailed variability metallurgical
extensions, including testwork is planned at ALS Perth to
the main geological support further studies.
interpretations and Detailed open pit and civils geotechnical
future drilling areas, studies are planned to support further
provided this information studies.
is not commercially Detailed hydrology studies are planned.
sensitive. Additional Mineral Resource, Ore Reserve
and grade control pattern drilling
is planned to update designs prior
to commencement of mining.
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