REG - Panthera Resources - Bido Drilling Results

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RNS Number : 3955P  Panthera Resources PLC  19 January 2026

The information contained within this announcement is deemed by the Company to
constitute inside information as stipulated under the UK Market Abuse
Regulation

 

 

19 January 2026

 

Panthera Resources Plc

("Panthera" or "the Company")

 

Bido Drilling Results

 

Gold exploration and development company Panthera Resources Plc (AIM:PAT),
with assets in West Africa and India, is pleased to announce that positive
results have been returned for Reverse Circulation ("RC") drilling samples
from the Bido Project in Burkina Faso. This RC drilling took place in the
second half of 2025 as announced on 18 July 2025, and represented limited,
shallow testing of a total of 5 targets. The delay in the final release of
information has been due to a combination of weather delays during the wet
season and several iterations of re-verifying assays using the Photon Assay
technique, as described below.

 

Highlights

·    Maiden exploration drilling programme at Kwademen has confirmed
historical zones of gold mineralisation

·    Targets 1 and 2

o KWD25-RC-001

§ 12m @ 0.2 g/t Au from surface

§ 18m @ 0.54 g/t Au from 72m

§ 2m sample loss from 78m

§ 1m @ 6.57 g/t Au from 80m

§ 1m @ 0.73 g/t Au from 81m

o KWD25-RC-017

§ 10m @ 0.72 g/t Au from surface

§ 5m @ 4.95 g/t Au from 35m

§ 1m @ 19.2 g/t Au from 36m

o KWD25-RC-003 intersected 24m @ 0.61 g/t from 26m including

§ 1m @ 8.25 g/t Au from 26m

§ 1m @ 3.41 g/t Au from 37m

·    Target 5

o KWD25-RC-014A intersected 4m @ 2.52 g/t Au from 34m including

§ 1m @ 3.94 g/t Au from 34m

§ 1m @ 5.38 g/t Au from 35m

 

Commenting on the results, Mark Bolton, Managing Director of Panthera said:

 

"The maiden drilling programme by Panthera at the Kwademen prospect has
delivered outstanding high-grade intersections within several broad zones of
mineralisation that remain open in multiple directions. This bodes well in a
strong, rising gold price environment."

 

About the Bido Project

 

The Company has now completed the earn-in obligations at Bido in Burkina Faso
and owns an 80% interest in the project. The Company may acquire the remaining
20% by expenditure of a further US$1,000,000 on exploration and development
within two years, subject to the vendor's rights of a buy-back right of 1%
interest in the Tenements and Associated Rights for the price of US$1,000,000.
A royalty will be payable to the vendor on all minerals produced by exercise
of rights under the Tenements which shall be calculated at the rate of 1% of
the net smelter returns (NSR) on all minerals extracted from the Properties
pursuant to the Tenements, inclusive of any withholding tax (if any) payable
in respect of those royalties and shall be paid quarterly. Payments via the
NSR will be capped at US$3 million in total.

 

The Bido permit in Burkina Faso (Figure 1) is located some 125km WSW of the
capital Ouagadougou. The tenement lies within the Boromo greenstone belt which
is principally composed of Paleoproterozoic Birimian terrain within the West
African Man Craton.  This belt also hosts the Poura gold deposit (1 to 2
Moz), situated about 50 km to the SSW of the area, as well as numerous gold
occurrences. The Perkoa VMS deposit is located about 35 km to the north of the
area.

 

The Kwademen Prospect (Figure 1) was originally identified from an analysis of
historical data from exploration undertaken in the 1980s, culminating in
trenching and diamond drilling.  This work was undertaken by BUVOGMI, the
national geological service of Haute Volta (former name of Burkina-Faso) under
financing of the United Nations Development Program (UNDP). It targeted base
metals and gold.

 

In that early historical work several interesting intervals were intersected
in different holes which were not followed up at the time, we understand for
different reasons, among which the more plausible is the ending of the
financing of the UNDP program. Exploration was then on 'ice' until resumed in
2014 when Panthera's joint-venture partner attracted foreign interest in
further exploration.

 

The company's experienced in-country and international geological team have
completed systematic geological mapping, data compilation, geochemical and
geophysical surveys and interpretation of the database to identify drill
targets, some of which represent the priority targets in this round of
exploration drilling.

 

Figure 1: Bido Project Location, Prospects and Geophysical Survey Grid
Locations

 

Drilling Programme

 

An RC drilling program targeting the Kwademen prospect has been completed with
19 holes completed for 1858.9 metres advance which includes several re-drilled
holes where original holes had to be abandoned due to weather and drilling
equipment issues. Drilling conditions were hard due to the advanced stage of
the rainy season and its particular wetness in 2025, with some holes
encountering strong underground water ingress. This, combined with equipment
failure and constraints, led to a very delayed completion of drilling.

 

The Kwademen prospect is located on the north-western part of the Bido
tenement limits (Figure 1). Panthera Resources started exploration work on the
area doing compilation work followed by soil sampling in 2018. The soil
sampling program consisted of sampling on east-west lines spaced of 200 m with
sampling repeated at 50m interval on each line. An Induced Polarized (IP)
survey was conducted in 2023 and consisted of a gradient survey exploring the
ground at a relatively constant depth of 50m followed by a Pole-Dipole survey
on some selected lines to help determining the depth of the anomalies
identified by gradient as long as determining the dip of the chargeable
structures. More recently and prior to the finalisation of this proposal for
drilling, a program of systematic mapping of all orpailleurs shafts and areas
of eluvial workings was completed.

 

A plan showing the location of the drilling and targets is shown in Figure 2
below, where Targets 1 to 5 are represented as Lines 1 to 5.

 

Figure 2: Plan View of the drilling at the Kwademen prospect

 

Drilling Results

 

Based on the results of the 2m samples analysis (analysed at SGS Laboratory in
Ouagadougou by a Fire Assay of a 50gm aliquot) received best results of the
drilling program are summarized in Table 1 below. The intervals were
re-assayed at 1 metre split intervals, also provided in Table 1.

 

The Company had concern that the potential for nuggety gold may occur in some
of the intersections and elected to re-assay the 1m splits using the
PhotonAssay method as provided by Intertek in Ghana, the intervals are also
provided in Table 1. The method analyses a 500gm split using sample
irradiation (reference - PhotonAssay - Chrysos Corporation
(https://chrysoscorp.com/photonassay/) ) the method involves "hitting samples
with high-energy X-rays, Chrysos PhotonAssay™ technology causes excitation
of atomic nuclei allowing enhanced analysis of gold, silver, copper and other
elements in as little as two minutes". The Company completed a comparison of
the analytical methods and found that no significant grade variations occurred
(see Chart 1 and Table 1 below).

 

 

Table 1: Best results of the 2025 drilling program

 

 HOLE           2 m splits (Fire Assay) best intercepts                                      Re-assay (Fire Assay) at 1 m splits best intercepts                          Re-assay (PhotonAssay) at 1 m splits best intercepts
 KWD25-RC-001   12 m @ 0.2 g/t Au from 0 m                                                   12 m @ 0.17 g/t Au from 0 m                                                  12 m @ 0.21 g/t Au from 0 m
 KWD25-RC-001   8 m @ 0.15 g/t Au from 36 m                                                  8 m @ 0.18 g/t Au from 36 m                                                  8 m @ 0.16 g/t Au from 36 m
 KWD25-RC-001   6 m @ 0.27 g/t Au from 56 m                                                  6 m @ 0.31 g/t Au from 56 m                                                  6 m @ 0.26 g/t Au from 56 m
 KWD25-RC-001   18 m @ 0.54 g/t Au from 72 m No chips recovery between 78 m and 80 m. 0 g/t  18 m @ 0.61g/t Au from 72 m No chips recovery between 78 m and 80 m. 0 g/t   18 m @ 0.72g/t Au from 72 m No chips recovery between 78 m and 80 m. 0 g/t
                assumed for this interval here although it is in the richer part of the      assumed for this interval here although it is in the richer part of the      assumed for this interval here although it is in the richer part of the
                mineralisation                                                               mineralisation                                                               mineralisation
 KWD25-RC-001   4 m @ 0.96 g/t from 126 m                                                    4 m @ 0.56 g/t from 126 m                                                    4 m @ 0.72 g/t from 126 m
 KWD25-RC-003   24 m @ 0.61 g/t Au from 18 m incl. 12 m @ 1.0 g/t Au from 26 m               24 m @ 0.72 g/t Au from 18 m incl. 12 m @ 1.2 g/t Au from 26 m               24 m @ 0.64 g/t Au from 18 m incl. 12 m @ 1.03 g/t Au from 26 m
 KWD25-RC-006   4 m @ 0.19 g/t Au from 24 m                                                  4 m @ 0.16 g/t Au from 24 m                                                  4 m @ 0.14 g/t Au from 24 m
 KWD25-RC-006   6 m @ 0.13 g/t Au from 34 m                                                  6 m @ 0.20 g/t Au from 34 m                                                  6 m @ 0.18 g/t Au from 34 m
 KWD25-RC-006   2 m @ 1.58 g/t Au from 46 m                                                  2 m @ 0.42 g/t Au from 46 m                                                  2 m @ 0.51 g/t Au from 46 m
 KWD25-RC-006   22 m @ 0.33 g/t Au from 62 m                                                 22 m @ 0.28 g/t Au from 62 m                                                 22 m @ 0.26 g/t Au from 62 m
 KWD25-RC-007   6 m @ 0.28 g/t Au from 32 m                                                  6 m @ 0.21 g/t Au from 32 m                                                  6 m @ 0.19 g/t Au from 32 m
 KWD25-RC-007   4 m @ 0.43 g/t Au from 44 m                                                  4 m @ 0.35 g/t Au from 44 m                                                  4 m @ 0.29 g/t Au from 44 m
 KWD25-RC-013   14 m @ 0.53 g/t Au from 32 m                                                 14 m @ 0.51 g/t Au from 32 m                                                 14 m @ 0.49 g/t Au from 32 m
 KWD25-RC-014A  4 m @ 2.52 g/t Au from 34 m incl. 2 m @ 4.73 g/t Au from 34 m                4 m @ 2.46 g/t Au from 34 m incl. 2 m @ 4.66 g/t Au from 34 m                4 m @ 2.58 g/t Au from 34 m incl. 2 m @ 4.93 g/t Au from 34 m
 KWD25-RC-017   10 m @ 0.72 g/t Au from 0 m                                                  10 m @ 0.40 g/t Au from 0 m                                                  10 m @ 0.41 g/t Au from 0 m
 KWD25-RC-017   8 m @ 0.68 g/t Au from 34 m                                                  8 m @ 3.12 g/t Au from 34 m incl. 1 m @ 19.2 g/t Au from 36 m repeated with  8 m @ 3.79 g/t Au from 34 m incl. 1 m @ 22.17 g/t Au from 36 m
                                                                                             Photon assay returned 22.17 g/t Au (see Table 2)
 KWD25-RC-017   4 m @ 0.24 g/t Au from 56 m                                                  4 m @ 0.23 g/t Au from 56 m                                                  4 m @ 0.17 g/t Au from 56 m
 KWD25-RC-017   6 m @ 0.31 g/t Au from 66 m (hole stopped at 72 m within mineralisation)     6 m @ 0.35 g/t Au from 66 m (hole stopped at 72 m within mineralisation)     6 m @ 0.22 g/t Au from 66 m (hole stopped at 72 m within mineralisation)

 

To verify repeatability of the samples collected at 2m intervals the Company
collected splits of mineralised zones at 1m intervals. The 1m splits were
initially analysed at SGS Laboratory in Ouagadougou by a Fire Assay of a 50g
aliquot. This more detailed sampling gave similar results to the original 2m
split sampling (Table 1). The exception being for an interval in hole
KWD25-RC-017 where resampling at 1 m intervals gave 5m @ 4.95 g/t Au from 35m
to 40m and included 36m to 37m @ 19.2 g/t Au. Note original 2m sample split
(Fire Assay) from 36m to 38m returned 1.03 g/t Au while re assay by Photon
Assay of the 1m interval, 36m to 37m, returned 22.17 g/t Au as shown in table
2 below.

 

Table 2: Comparison of results in hole KWD25-RC-017

 

 

 

At Target 1 (testing continuity of historical holes where gold intervals of 24
m @ 1.38 g/t Au from 143 m, 9 m @ 0.51 g/t Au and 10 m @ 0.57 g/t Au reported
in three holes):

•    Hole KWD-RC-001 started directly within a gold intersection with 12
m @ 0.2 g/t from 0 m within colluvium and saprolite horizon. Two other gold
zones were intersected at 36 m with 8 m @ 0.15 g/t Au within a tuff with minor
patchy pyrite and at 56 m with 6 m @ 0.27 g/t Au within tuff with local
pyrrhotite and weak pervasive carbonate alteration. A further zone was
intersected from 72 m over 18 m with an average of 0.54 g/t, including 12 m @
0.7 g/t Au, within a tuff with pyrite and pyrrhotite (0.5% to 2%) and weak
pervasive chlorite and carbonate alteration. The interval from 80 m to 82 m
returned 3.2 g/t Au and the interval 126 m with 0.96 g/t Au over 4 m (Figure
3).

•    Hole KWD25-RC-017 (Figure 4) tested the Target 1 zone for the
continuity of the mineralisation about 100 m south of KWD25-RC-001. The hole
also started directly within the gold mineralisation with 10 m @ 0.72 g/t Au
from surface in a laterite with laminated and smoky quartz fragments horizon.
This was followed by 8 m @ 0.68 g/t Au from 34 m within a tuff with laminated
quartz veinlets and weakly pervasive chlorite alteration. The interval from 56
m returned 4 m @ 0.24 g/t Au with patchy pyrrhotite and quartz stringers.
Mineralisation was also intersected from 66 m to 72 m (where the hole stopped
due technical issues). This interval reports 6 m @ 0.31 g/t Au from 66 m. Both
KWD25-RC-001 and KWD25-RC-017 started directly within gold mineralisation
demonstrating the extension of the mineralisation may extend to the east
(large soil anomaly) as shown on Figure 2.

 

Figure 3: Section View of Target 1 and Section view Hole KWD-RC-001

 

Figure 4: Section View of Target 1 and Section view Hole KWD-RC-017

 

Target 2 (testing combined geophysical (IP) and soil anomalies and coincident
historical drill results such as 16 m @ 1.07 g/t Au, 11 m @ 0.40 g/t Au and 13
m @ 0.53 g/t Au) was drilled with 4 holes (KWD25-RC-002, KWD25-RC-003,
KWD25-RC-004 and KWD25-RC-005), Figure 5.

•    Hole KWD25-RC-003 intersecting 24 m @ 0.61 g/t from 26 m was
intersected in this hole and this include 12 m @ 1.0 g/t Au within a
dacite/tuff horizon with local patchy pyrite and pyrrhotite and quartz
stringers.

 

Figure 5: Section View of Target 2 and Section view Holes KWD-RC-002 to
KWD-RC-005

 

Target 3 (testing an area to include follow up of a RAB hole drilled in 2014
reporting 13 m @ 22.11 g/t Au to the end of hole (reference the company's AIM
Admission Document)) included drilling of two holes (Figure 6),

•    KWD25-RC-006 returned a gold interval of 2 m @ 1.58 g/t from 46 m
within a tuff with minor pyrite, pyrrhotite and weak pervasive chlorite and
carbonate alteration followed by a broader zone of 22 m @ 0.33 g/t Au from 62
m within the same lithological unit. Other less relevant intervals in this
hole were to 4 m @ 0.19 g/t Au from 24 m and 6 m @ 0.13 g/t Au from 34 m.

•    Hole KWD25-RC-007 was drilled to the east of KWD25-RC-006 and
intersected 6 m @ 0.28 g/t Au from 32 m within and andesite with patchy pyrite
and pyrrhotite followed by 4 m @ 0.43 g/t Au from 44 m within the same
lithological unit.

The hole KWD25-RC-006 successfully intersected a zone of gold mineralisation
at depth below a previously reported RAB hole KWRAB23 drilled in 2014
(reference the Company's AIM Admission Document) that reported a gold interval
of 13 m @ 22.11 g/t Au from 20 m. This included 1 m @ 45.5 g/t from 21 m and 1
m @ 9.79 g/t from 25 m. The new drilling has successfully identified this vein
system to dip westwards, thus further focused testing of this potentially
higher-grade vein system, and its strike extent will be planned.

 

Figure 6: Section View of Target 3 and Section view Holes KWD-RC-006 and
KWD-RC-007

 

Target 4 (axis of high chargeability IP anomalies and gold in soil anomalies)
was tested with 5 drill holes (KWD25-RC-008 to KWD25-RC-12): no significant
gold intersections were returned despite the moderate to high presence of
alteration pyrite and pyrrhotite, in some relevant intervals. It was elected
to send selected intervals of these holes to Ghana for PhotonAssay as a
further check methodology, but results were comparable to the original fire
assay.

 

Target 5 (an area where a high chargeability IP anomaly is located underneath
a recently dug and extensive line of orpailleurs shafts) was partly tested
with 4 holes, KWD25-RC-013 to KWD25-RC-016 (Figure 7). Significant
intersections were:

•    KWD25-RC-013 returned 14 m @ 0.53 g/t from 32 m in quartz stringers
and weak pervasive chlorite.

•    KWD25-RC-014A returned 4 m @ 2.52 g/t Au from 34 m, including 2 m @
4.73 g/t Au, in graphitic shist with laminated smoky quartz veining and
pervasive carbonate alteration. A further interval of 8 m @ 0.29 g/t Au from
54 m within graphitic shist with smoky quartz veining, local patchy pyrite,
pyrrhotite and pervasive chlorite alteration was returned.

•    Unfortunately, holes KWD25-RC-015 and KWD25-RC-016 did not return
significant gold intersections.

 

Figure 7: Section View of Target 5 and Section view Holes KWD-RC-013 to
KWD-RC-016

 

Analysis of Results

 

Kwademen is part of the Bido/Boromo greenstone belt (often also linked with
the Poura belt), a Paleoproterozoic Birimian volcano‑sedimentary terrane
that hosts multiple gold and base‑metal deposits including Poura and Perkoa.
Kwademen is located within a shear corridor, where tholeiitic to
calc‑alkaline basalts, andesites and related volcano‑sedimentary rocks are
strongly deformed and metamorphosed to lower‑greenschist facies 1 .

 

Gold at and near Kwademen is described 2  as shear‑hosted orogenic
mineralisation, with alteration and sulphide dissemination
(biotite‑chlorite, carbonate, oxides) associated with deformed volcanic
rocks in the Kwademen‑Baguiomo shear zone and the Kwademen mineralisation is
considered to be localized in these shears, with gold pits and artisanal
workings aligned along the main shear direction. In addition to gold, the
Kwademen prospect has some potential for polymetallic (Cu‑Zn±Pb±Au) style
mineralisation. This style is described 3  as a volcanogenic massive
sulphide-type (VMS), best represented by the Perkoa deposit; the latter is not
an immediate target for our exploration at this time.

 

This drill programme has supported our exploration model with the
identification of wide zones of quartz veining, alteration (pervasive
carbonate, chlorite and silica) and associated sulphides coincident with the
wider gold intersections. Sulphides are generally represented by boxwork
textures or limonite replacing sulphides, but occasionally fresh pyrite and/or
arsenopyrite has been logged.

The limited programme of drilling has successfully upgraded 4 of the 5 targets
tested in this programme with wide but low-grade gold intersections with
identified along strike extension potential.

 

This successful programme of drilling will provide follow up locations for
detailed future drilling work.

 

Contacts

 

Panthera Resources PLC

Mark Bolton (Managing
Director)
+61 411 220 942

 
contact@pantheraresources.com

 

Allenby Capital Limited (Nominated Adviser & Joint
Broker)             +44 (0) 20 3328 5656

John Depasquale / Vivek Bhardwaj (Corporate
Finance)

Kelly Gardiner (Sales & Corporate Broking)

 

VSA Capital Limited (Joint
Broker)
+44 (0) 20 3005 5000

Andrew Monk / Andrew Raca

 

AlbR Capital Limited (Joint
Broker)
+44 (0) 20 7399 9400

Colin
Rowbury

 

Subscribe for Regular Updates

 

Follow the Company on Twitter at @PantheraPLC
(https://twitter.com/PantheraPlc)

 

For more information and to subscribe to updates visit: pantheraresources.com
(http://pantheraresources.com)

 

Qualified Persons

The technical information contained in this disclosure has been read and
approved by Ian S Cooper (BSc, ARSM, FAusIMM, FGS), who is a qualified
geologist and acts as the Qualified Person under the AIM Rules - Note for
Mining and Oil & Gas Companies.  Mr Cooper is a geological consultant to
Panthera Resources PLC.

 

 

Glossary

 

 Au:                   The chemical element for Gold

 Diamond Core          Diamond core drilling uses a diamond cutting bit, which rotates at the end of

Drilling:            a steel rod (tube) allowing for a solid column of rock to be recovered from

                     the tube at the surface.

 g/t:                  Grammes per Tonne (Metric)

 JORC or JORC Code:    Australasian Code for Reporting of Mineral Resources and Ore Reserves of
                       December 2012 ("JORC Code") as prepared by the Joint Ore Reserves Committee of
                       the Australasian Institute of Mining and Metallurgy. Terms including Measured,
                       Indicated and Inferred Resources as defined therein

 RC Drilling:          Reverse Circulation drilling, or RC drilling, uses rods with inner and outer
                       tubes, the drill cuttings are returned to surface inside the rods. The
                       drilling mechanism is a pneumatic reciprocating piston known as a hammer
                       driving a tungsten-steel drill bit.
 IP:                   Induced polarization (IP) is a geophysical imaging technique used to identify
                       the electrical chargeability of subsurface materials

 Fire Assay or FA:     Fire assay method has been practiced since ancient times and remains the
                       industry-standard technique for determining gold content in all sample types.
                       This well-understood technique provides accurate results across geological
                       sample types. However, practiced skill is essential to achieving a successful
                       fire assay. A range of fire assay methods are available with 30g or 50g sample
                       aliquots taken after a larger representative sample has been crushed and
                       pulverised for homogenisation. Multiple options for detection ranges to suit
                       the needs of the project.
 PhotonAssay:          The method analyses a 500gm split using sample irradiation (reference -
                       PhotonAssay - Chrysos Corporation (https://chrysoscorp.com/photonassay/) ) the
                       method involves "hitting samples with high-energy X-rays, Chrysos
                       PhotonAssay™ technology causes excitation of atomic nuclei allowing enhanced
                       analysis of gold, silver, copper and other elements in as little as two
                       minutes".

 

Forward-looking Statements

This news release contains forward-looking statements that are based on the
Company's current expectations and estimates. Forward-looking statements are
frequently characterised by words such as "plan", "expect", "project",
"intend", "believe", "anticipate", "estimate", "suggest", "indicate" and other
similar words or statements that certain events or conditions "may" or "will"
occur. Such forward-looking statements involve known and unknown risks,
uncertainties and other factors that could cause actual events or results to
differ materially from estimated or anticipated events or results implied or
expressed in such forward-looking statements. Such factors include, among
others: the actual results of current exploration activities; conclusions of
economic evaluations; changes in project parameters as plans continue to be
refined; possible variations in ore grade or recovery rates; accidents, labour
disputes and other risks of the mining industry; delays in obtaining
governmental approvals or financing; and fluctuations in metal prices. There
may be other factors that cause actions, events or results not to be as
anticipated, estimated or intended. Any forward-looking statement speaks only
as of the date on which it is made and, except as may be required by
applicable securities laws, the Company disclaims any intent or obligation to
update any forward-looking statement, whether as a result of new information,
future events or results or otherwise. Forward-looking statements are not
guarantees of future performance and accordingly, undue reliance should not be
put on such statements due to the inherent uncertainty therein.

 

 

**ENDS**

 

 1  Ouiya, P. , Tarnagda, A. and Fozing, M. (2024) Characteristics of Gold
Mineralization at the Baguiomo Gold Panning Site, Koudougou Region, Burkina
Faso, West Africa. Open Journal of Geology, 14, 1-18. doi:
10.4236/ojg.2024.141001.

 

 2  Tarnagda, F., Ouiya, P., & Sawadogo, S. (2023). Identifying Areas of
High Gold Potential Using Geochemical Prospecting Methods: The Tenado area in
the Boromo Birimian Belt, West-Central Burkina Faso, West Africa. European
Scientific Journal, ESJ, 24, 599.

 

 3  Cheik Abba Cissé Ouangaré, Séta Naba, Patrick Lachassagne,

Enhancement of the geological mapping in weathered plutonic and metamorphic
rocks areas using village water supply wells data (lithology and
hydrochemistry), Heliyon, Volume 10, Issue 22, 2024,

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