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RNS Number : 4748L Power Metal Resources PLC 15 December 2025
15 December 2025
Power Metal Resources PLC
("Power Metal" or the "Company")
Block 8 Oman: Drilling Programme Results
Power Metal Resources PLC (AIM: POW, OTCQB: POWMF), the London listed
exploration company and project incubator with a global project portfolio, and
its majority held subsidiary Power Arabia Ltd ("Power Arabia"), are pleased to
provide an update on the maiden drilling programme on the Block 8 concession
in Oman ("Block 8" or the "Project").
Highlights:
· Maiden reconnaissance diamond core drilling programme completed in
October 2025, with eight drill holes for a total meterage of 724.45 metres
("m") drilled.
· Identified lithological units, alteration, brecciation and
mineralisation consistent with copper-dominant (Cyprus-type) Volcanogenic
Massive Sulphide ("VMS")(1, 2).
· All holes intersected prospective lithological units, including basalt
and andesite with associated carbonate, chlorite and epidote alteration.
· Highlight downhole depth intercepts of:
· 1.04% Copper ("Cu") over 1.5m (hole AM25DD001 from 95.5-97m within
wider zone returning 0.52% Cu from 95.5-99.0m);
· 0.36% Cu over 1m (AM25DD001 from 72-73m, within a broader elevated Cu
zone from 68-77m);
· 0.35% Cu over 4m (AM25DD001 from 80-84m, with up to 0.56% Cu from
80-81m);
· 0.19% Cu over 4m (AM25DD002 from 85-89m);
· Elevated Cu, lead ("Pb") and zinc ("Zn") results over 18 m (AM25DD003
from 35-53m, associated with a sulphide stockwork in a fault zone); and
· 1.1% Zn over 1m (AM25DD006 from 51-52m, plus elevated Cu and Zn from
51-58m).
Block 8 is the subject of an agreement for Power Metal to earn a 12.5% stake
in the Project held by ASX-listed Alara Resources Limited ("Alara") and Awtad
Copper LLC ("Awtad Copper"). The exploration work, led and undertaken by the
Power Arabia technical team, commenced in October 2024 following the signing
of a formal and legally binding agreement on 25 October 2024.(3, 4)
The drilling programme completes the initial 12.5% earn-in.
Sean Wade, Chief Executive Officer of Power Metal Resources PLC, commented:
"The results of the maiden drilling programme are very encouraging and confirm
our view that this is a prospective area that has been under-explored. The
completion of the programme marks the fulfilment of the agreed $740,000 spend
to earn a 12.5% stake in Block 8.
"I look forward to updating the market further as we move into the next phase
of workstreams with additional trenching and drilling programmes that will
enhance our understanding of the results and the mineralised intersects."
Atmavireshwar Sthapak, Managing Director of Alara Resources said:
"We are very encouraged by the results of this maiden drilling programme at
Block 8. The identification of VMS-style mineralisation, strong alteration
signatures and structural features across all drill holes confirms the
robustness of the geological model developed through the Power Metals
exploration work. These early results highlight the potential of Block 8 to
host Cyprus-type copper mineralisation, and they provide a solid foundation
for advancing the next phase of exploration.
We look forward to continuing our collaboration with Power Metal and Awtad
Copper as we build further momentum on this promising project."
Block 8
Block 8 is located approximately 130 kilometres ("km") west of Muscat in Oman
and encompasses a contiguous area of 497 km(2) (Figure 1). The concession
includes a section of the Semail Ophiolite that is prospective for
copper-dominant (Cyprus-type) VMS mineralisation. Power Arabia's exploration
activities have included spectral remote sensing, stream sediment, soil and
rock chip sampling, trenching and sampling, gravimetric surveying, petrography
and X-Ray Diffraction ("XRD") analysis.
Figure 1: Location of Block 8 Concession, Oman
Drilling programme
The initial drilling targets were mainly based on geological observations,
magnetic and gravimetric data, and trenching results. However, the locations
were ultimately adjusted in response to observations as the programme, which
contained eight holes totalling 724.45m, developed.
The drillhole locations and parameters are shown in Figure 2 and summarised in
Table 1 respectively.
Figure 2: Block 8 Drillhole Locations Relative to Gravimetric Geophysics
Results
Table 1: Block 8 Drillhole Summary
Drillhole ID Easting Northing Elevation (m) Azimuth (deg) Inclination (deg) Length (m)
(UTM 40N) (UTM 40N)
AM25DD001 554,348 2,598,839 202.36 120 -50 109.45
AM25DD002 554,411 2,598,807 200.97 120 -50 110
AM25DD003 554,356 2,598,770 204 225 -50 70.9
AM25DD004 554,371 2,599,075 195.3 120 -50 80
AM25DD005 554,440 2,599,046 194.4 120 -50 100
AM25DD006 554,292 2,598,833 210 225 -50 74
AM25DD007 554,751 2,600,005 192 120 -50 80
AM25DD008 554,355 2,598,770 204 225 -65 100
TOTAL: 724.35
Drillhole observations
The drilling intersected a volcanic succession predominantly consisting of
intercalated andesite and basalt units. Andesite units ranged in thickness
from 0.12 to 11.1m (averaging 3.22m), and basalt units ranged in thickness
from 0.13 to 12.95m (averaging 2.0m). Some of the basalt units included
pillows, substantiating subaqueous deposition and favourable genetic
conditions for the formation of massive sulphide mineralisation.
Propylitic alteration, including carbonate, chlorite and epidote, was apparent
in almost all drillholes and particularly associated with basaltic units.
Faulting and brecciation were also common and evident in all drillholes.
Breccias ranged in thickness from 0.2 to 13.5m (averaging 3.82m) and some were
associated with alteration (silica, carbonate, chlorite, epidote and
hematite).
Significant sulphides, mainly pyrite, were intersected in six of the eight
drillholes. The pyrite occurred as disseminations, veinlets and in
semi-massive form (Figures 3-5).
Figure 3: Brecciated Semi-Massive Pyrite in Drill Core (AM25DD001 at 95.7m)
Figure 4: Brecciated and Colloform Pyrite in Drill Core (AM25DD001 from 95.5m)
Figure 5: Semi-massive Pyrite and Quartz Breccia/Stockwork Drill Core
(AM25DD003)
Pyrite mainly occurred within the andesite and basalt units and in the
presence of propylitic alteration, although some of the faults and breccias
also included pyrite disseminations and veinlets.
Drillhole sampling and results
A total of 156 half-core samples were cut using a diamond saw with 11 Quality
Assurance ("QA") samples distributed throughout the batch. All samples were
prepared and analysed by ALS Arabia Biyaq in Oman.
Drillhole AM25DD001 included up to 1.04% Cu over 1.5m (from 95.5-97m downhole
depth) corresponding to faulted dolerite within a wider zone returning 0.52%
Cu over 3.5m (from 95.5-99m). Other intersections included 0.36% Cu over 1m
(from 72-73m) and 0.35% Cu over 4m (from 80-84m). Half of the samples from the
drillhole (36 of 72) returned Cu values > 100 ppm Cu (the average abundance
for basalts(5)) and correspond to elevated iron z-scores (z-scores indicate
how many standard deviations a result is from the mean of a distribution and
is used to assess anomalous values).
Drillhole AM25DD002 included up to 0.19% Cu over 4m (from 85-89m downhole) in
basalt.
Drillhole AM25DD003 included up to 0.18% Cu over 1m (from 42-43m downhole)
within a stockwork zone.
Drillhole AM25DD006 included up to 1.1% Zn over 1m (from 51-52m downhole).
Tabulated drillhole results are provided in Table 2 below.
Sections for drillholes AM25DD001 and 2, and AM25DD003 and 8 are shown in
Figures 6 and 7 respectively.
Figure 6: Section for Drillholes AM25DD001 and AM25DD002 (looking north)
Figure 7: Section for Drillholes AM25DD003 and AM25DD008, plus Trench AM24TR02
(looking west)
Conclusions
The drillhole observations and results identified some significant sulphide
mineralisation in what is interpreted to be the peripheral zone of a
mineralised system. The >1% Cu intersection in hole AM25DD001, along with
the other geochemically anomalous zones, offer great encouragement and targets
for the next phases of work.
The next phases of work include a full review of all results to better
understand the geological associations with mineralisation, with an emphasis
on the breccia units. This would facilitate the planning of a follow-up
trenching and drilling programme.
Some additional sampling on the remaining core is also planned. This includes
sampling the rest of AM25DD006, hole AM25DD007 (located over 1km to the north
of hole AM25DD001), as well as potentially some intervals of the as yet
unsampled holes AM25DD004, 5 and 7 (that contain alteration and some observed
mineralisation).
Table 2: Highlighted Drill Hole Intersections
Drill Hole ID Sample ID Downhole Intersection Lithology Selected Assay Results (*)
From To Cu Zn
(m) (m) (ppm) (ppm)
AM25DD001 533006 43 44 Basalt 155 53
AM25DD001 533007 44 45 Basalt 44 49
AM25DD001 533008 45 46 Basalt 178 53
AM25DD001 533009 46 47 Andesite 191 55
AM25DD001 533010 47 48 Andesite 403 65
AM25DD001 533011 48 49 Andesite 118 66
AM25DD001 533025 61 62 Andesite 122 45
AM25DD001 533026 62 63 Andesite 171 47
AM25DD001 533027 63 64 Andesite 91 50
AM25DD001 533028 64 65 Basalt 122 49
AM25DD001 533029 65 66 Basalt 92 47
AM25DD001 533030 66 67 Basalt 96 44
AM25DD001 533031 67 68 Basalt 118 58
AM25DD001 533032 68 69 Basalt 160 67
AM25DD001 533033 69 70 Basalt 291 70
AM25DD001 533034 70 71 Basalt 231 76
AM25DD001 533035 71 72 Basalt 86 82
AM25DD001 533036 72 73 Andesite 3560 101
AM25DD001 533037 73 74 Andesite 303 67
AM25DD001 533038 74 75 Andesite 139 64
AM25DD001 533039 75 76 Andesite 90 66
AM25DD001 533041 76 77 Andesite 254 57
AM25DD001 533042 77 78 Andesite 85 65
AM25DD001 533043 78 79 Andesite 62 56
AM25DD001 533044 79 80 Andesite 85 64
AM25DD001 533045 80 81 Andesite 5630 105
AM25DD001 533046 81 82 Andesite 2860 77
AM25DD001 533047 82 83 Basalt 3800 104
AM25DD001 533048 83 84 Basalt 1520 87
AM25DD001 533049 84 85 Basalt 127 67
AM25DD001 533056 90 91 Andesite 126 71
AM25DD001 533057 91 92 Basalt 68 69
AM25DD001 533058 92 93 Basalt 111 75
AM25DD001 533059 93 94 Breccia 43 81
AM25DD001 533061 94 95 Andesite 44 103
AM25DD001 533062 95 95.5 Breccia 25 74
AM25DD001 533063 95.5 96 Dolerite 10000 70
AM25DD001 533064 96 97 Fault 10850 78
AM25DD001 533065 97 98 Dolerite 149 60
AM25DD001 533066 98 99 Fault 2160 136
AM25DD001 533067 99 100 Andesite 212 86
AM25DD001 533068 100 101 Fault 85 72
AM25DD001 533069 101 102 Andesite 601 101
AM25DD001 533070 102 103 Basalt 34 86
AM25DD001 533071 103 104 Basalt 688 62
AM25DD001 533072 104 105 Andesite 115 71
AM25DD001 533073 105 106 Andesite 326 70
AM25DD001 533074 106 107 Andesite 34 61
AM25DD001 533075 107 108 Basalt 212 65
AM25DD001 533076 108 109 Andesite 63 64
AM25DD002 533079 83 84 Basalt 100 73
AM25DD002 533081 84 85 Basalt 114 69
AM25DD002 533082 85 86 Basalt 1580 67
AM25DD002 533083 86 87 Basalt 2950 63
AM25DD002 533084 87 88 Basalt 2080 74
AM25DD002 533085 88 89 Basalt 853 78
AM25DD002 533086 89 90 Basalt 95 73
AM25DD002 533087 90 91 Basalt 89 81
AM25DD002 533088 91 92 Basalt 71 66
AM25DD002 533089 92 93 Basalt 354 53
AM25DD002 533093 96 97 Fault 221 40
AM25DD002 533094 97 98 Fault 129 53
AM25DD002 533095 98 99 Fault 20 53
AM25DD002 533096 99 100 Fault 120 45
AM25DD003 533106 35 36 Fault 223 232
AM25DD003 533107 36 37 Fault 160 381
AM25DD003 533108 37 38 Fault 141 451
AM25DD003 533109 38 39 Fault 402 707
AM25DD003 533110 39 40 Fault 337 257
AM25DD003 533111 40 41 Stockwork 424 359
AM25DD003 533112 41 42 Stockwork 852 615
AM25DD003 533113 42 43 Sulphide 1805 551
AM25DD003 533114 43 44 Stockwork 151 566
AM25DD003 533115 44 45 Stockwork 34 317
AM25DD003 533116 45 46 Stockwork 251 92
AM25DD003 533117 46 47 Stockwork 125 641
AM25DD003 533118 47 48 Stockwork 93 216
AM25DD003 533119 48 49 Stockwork 208 1200
AM25DD003 533121 49 50 Stockwork 251 441
AM25DD003 533122 50 51 Stockwork 499 508
AM25DD003 533123 51 52 Fault 263 469
AM25DD003 533124 52 53 Fault 129 973
AM25DD003 533125 53 54 Breccia 41 207
AM25DD003 533126 54 55 Basalt 45 135
AM25DD003 533127 55 56 Basalt 67 129
AM25DD006 533159 51 52 Breccia 568 11050
AM25DD006 533161 52 53 Breccia 206 1775
AM25DD006 533162 53 54 Breccia 91 271
AM25DD006 533163 54 55 Breccia 105 388
AM25DD006 533164 55 56 Breccia 179 1855
AM25DD006 533165 56 57 Breccia 87 251
AM25DD006 533166 57 58 Basalt 501 289
AM25DD008 533144 83 84 Fault 135 198
AM25DD008 533145 84 85 Breccia 96 106
AM25DD008 533146 85 86 Breccia 77 238
Table notes: * Assay data by ALS Laboratories method ME-ICP61. 10,000 parts
per million (ppm) = 1.0 %. Cu or Zn intersections > 1,000 ppm
highlighted in bold. AM25DD006 partially sampled and drillholes AM25DD004, 5
& 7 not yet sampled.
References
1: Franklin, J. M., Gibson, H. L., Jonasson, I. R. and
Galley, A. G. 2005. Volcanogenic massive sulphide deposits. Economic Geology.
100(th) Anniversary Volume. Pp. 523-560.
2: Taylor, C. D., Zierenberg, R. A., Goldfarb, R. J.,
Kilburn, J. E., Seal, R. R., Kleinkopf, M.D. and Du Bray, E.A., 1995.
Volcanic-associated massive sulfide deposits. United States Geological
Survey, America. Open-File Report. Pp. 137-144.
3: Company announcement, Non-binding Heads of Terms
signed with Alara Resources & Awtad Copper, dated 11 September 2024
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/xpd67mx
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/xpd67mx)
).
4: Company announcement, Agreement with Alara Resources
& Awtad Copper, dated 25 October 2024
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/rd8z59w
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/rd8z59w)
).
5: Taylor, S. R. 1964. Abundance of chemical elements in
the continental crust: a new table. Geochemica et Cosmochimica Acta. Vol. 38.
Pp. 1273-1285.
QUALIFIED PERSON STATEMENT
The technical information contained in this disclosure has been read and
approved by Mr Nick O'Reilly (MSc, DIC, MIMMM QMR, MAusIMM, FGS), who is a
qualified geologist and acts as the Qualified Person under the AIM Rules -
Note for Mining and Oil & Gas Companies. Mr O'Reilly is a Principal
Consultant working for Mining Analyst Consulting Ltd which has been retained
by Power Metal Resources PLC to provide technical support.
For further information please visit https://www.powermetalresources.com/
(https://www.powermetalresources.com/) or contact:
Power Metal Resources PLC
Sean Wade (Chief Executive Officer) +44 (0) 20 3778 1396
SP Angel Corporate Finance LLP (Nomad and Joint Broker)
Ewan Leggat/Jen Clarke +44 (0) 20 3470 0470
Tamesis Partners LLP (Joint Broker)
Richard Greenfield/Charlie Bendon +44 (0) 20 3882 2868
BlytheRay (PR Advisors)
Tim Blythe/Alastair Roberts +44 (0) 20 7138 3204
powermetalresources@blytheray.com
NOTES TO EDITORS
Power Metal Resources PLC (AIM: POW, OTCQB: POWMF) is a London-listed metals
exploration company which finances and manages global resource projects and is
seeking large scale metal discoveries.
The Company has a principal focus on opportunities offering district scale
potential across a global portfolio including precious, base and strategic
metal exploration in North America, Africa, Saudi Arabia, Oman and Australia.
Project interests range from early-stage greenfield exploration to later-stage
prospects currently subject to drill programmes.
Power Metal will develop projects internally or through strategic joint
ventures until a project becomes ready for disposal through outright sale or
separate listing on a recognised stock exchange thereby crystallising the
value generated from our internal exploration and development work.
Value generated through disposals will be deployed internally to drive the
Company's growth or may be returned to shareholders through share buy backs,
dividends or in-specie distributions of assets.
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