TIDMPOW
RNS Number : 0283G
Power Metal Resources PLC
21 July 2021
21 July 2021
Power Metal Resources PLC
("Power Metal" or the "Company")
Botswana Molopo Farms Complex - Exploration Update
Proof-of-Concept Exploration Holes Recently Completed Confirm
the Presence of Primary Magmatic Sulphides at Molopo Farms Complex
Project
Power Metal Resources PLC (LON:POW) the AIM listed metals
exploration and development company is pleased to announce an
exploration update at the Kalahari Key Mineral Exploration Pty Ltd
("Kalahari Key" or "KKME") Molopo Farms Complex Project (the
"Project" or "MFC Project"), which is prospective for magmatic
intrusion-hosted massive and disseminated nickel-copper sulphide
and platinum-group element ("PGE") mineralisation in mining
friendly Botswana.
Power Metal currently has a 40% direct MFC Project interest as
well as an 18% shareholding in Kalahari Key, for a combined
effective economic interest of 50.8%.
Christian Schaffalitzky, Chairman of Kalahari Key,
commented:
"The MFC Project is transected by the Thabazimbi-Murchison
lineament ("TML"), a major fault system which trends easterly and
is believed by Kalahari Key to be the same structure which
controlled the emplacement of magma within the highly prolific
Bushveld Igneous Complex ("BIC") located in South Africa. The BIC
is one of the world's major sources of nickel and platinum group
metals ("PGMs").
By extension, the TML is believed to be the feeder for the
Molopo Farms Complex ("MCF"), and thus a target for a Voisey's Bay
style major nickel deposit. A feeder zone structure is interpreted
to be close to hole K1-6 and extends north-eastwards to the edge of
the licence area.
Recently completed proof-of-concept drilling by Kalahari Key,
including three widely spaced diamond drillholes targeting
large-scale conductive electromagnetic ("EM") geophysics anomalies,
has identified in hole K1-6 the highest nickel grades to date
within the MFC. Significantly, thin section analysis of select
drill intercepts has identified primary magmatic sulphide
mineralisation including pentlandite and chalcopyrite.
With several targets to be followed up, the work plan is still
being finalised and the priorities set."
Paul Johnson, Chief Executive Officer of Power Metal Resources
plc, commented:
"The results to date from the Phase I drill programme at the MFC
Project have successfully demonstrated the validity of the
geological model developed by our operating partner Kalahari Key,
which has led to the discovery of primary nickel-copper and PGE
mineralisation.
Further technical review of the Phase I exploration results is
ongoing, and we look forward to providing further information in
this regard.
The aim of our venture at the MFC project is the discovery of a
major nickel deposit, and we have clearly taken a number of
important steps forward with recent exploration. Now we need to
finalise the technical review of the work done thus far, and
implement next stage exploration work including a Phase II drill
programme."
PROJECT BACKGROUND:
The MFC Project is a district scale exploration opportunity
located in southwestern Botswana.
After extensive preparatory exploration work conducted over the
previous five years by Kalahari Key, including airborne and
ground-based Electro Magnetic ("EM") surveys which identified a
number of highly prospective kilometre-scale conductive targets,
the Project was suitably advanced to commence proof-of-concept
drilling late in 2020.
The Phase I diamond drilling commenced at the MFC Project in
October 2020 with three holes completed. Due to the size of the
Project and prospective conductors identified by the EM surveys,
the drilling was conducted as proof-of-concept in order to
determine if the conditions within the magmatic system were ideal
for the formation of primary magmatic Ni-Cu sulphides, similar to
those found within the Bushveld Igneous Complex located along
strike to the east.
Significantly, examination of the three proof-of-concept
drillholes has successfully identified a magmatic feeder zone which
is prospective for the accumulation of Ni/PGE sulphides within the
MFC project.
The assay results for core samples submitted from hole KKME 1-14
are outlined below. These results represent the second batch of
assay results for the MCF Project and continue to build on the
geological understanding of the MFC Projects magmatic feeder zones
following the significant Ni-Cu intersections reported previously
from drillhole KKME 1-6 (announced 8 April 2021).
DRILL RESULTS:
KKME 1-6
The assay results from angled diamond drill hole KKME 1-6
drilled to a total depth of 597.8 were previously reported on 8
April 2021 and are outlined in table 1 below.
Four select intervals from drillhole KKME 1-6 were analysed at
the Scientific Services Geological Laboratories ("SCISERV")
laboratory in Cape Town, South Africa which include 292.7 - 297.5m,
308.5 - 313.2m, 501.8 - 529.1m, and 585.0 - 597.8m.
Significant nickel intersections (1) include:
-- 4.8m @ 0.2% Ni from 292.7m
-- 4.1m @ 0.49% Ni from 309m, including 1.6m @ 0.72% Ni from 309.6m
-- 16.7m @ 0.16% Ni from 501.8m
-- 10.9m @ 0.13% Ni from 518.2m
-- 3.4m @ 0.28% Ni from 594.4m to end of hole at 597.8m (mineralisation remains open at depth)
Individual samples were also sent to the University of
Witwatersrand for thin section mineralogical analysis. The results
of this analysis, set out below, successfully identified the
presence of primary pentlandite, secondary nickel sulphide and
chalcopyrite mineralisation within three drill core samples from
KKME 1-6:
-- IMK-05139 (0.44m pyroxenite sample from 310m down-hole depth)
assayed at 6,999ppm Ni (0.70% Ni) from a primary magmatic,
pentlandite-bearing, assemblage.
-- IMK-05149 (0.58m pyroxenite sample from 295m down-hole depth)
assayed at 6,606ppm Ni (0.66% Ni).
-- IMK-05153 (0.54m pyroxenite sample from 297m down-hole depth)
assayed at 2,244ppm Ni (0.22% Ni).
-- Both IMK-05149 and IMK-05153 contained primary pentlandite
within predominant secondary nickel sulphides, arsenides and
alloys.
KKME 1-14
The assay results from angled diamond drill hole KKME 1-14
drilled to a total depth of 515.8m are outlined in table 2
below.
Four select intervals from drillhole KKME 1-14 were analysed at
the SCISERV laboratory which include 180.0 - 188.8m, 192.2 -
201.2m, 207.9 - 208.5m and 475.4 - 483.22m.
Significant nickel intersections (1) include:
-- 6.0m @ 0.17% Ni from 180.0m in harzburgite rock immediately above a fault zone at 186m; and
-- 1.0m @ 0.11% Ni from 194.0m in serpentinite with a partial
breccia texture within an intra-fault zone totalling 9m @ 0.07%Ni
between 192m and 201m downhole.
The drilling intersected the ultramafic rocks of the Molopo
Farms Complex directly below 40m of Kalahari sand and duricrust
cover and continued to a faulted contact with Transvaal Supergroup
quartzite units to a downhole depth of 205.5m. The hole remained in
Transvaal rocks through to its end at 515.8m downhole depth.
The anomalous nickel mineralisation identified at shallow depths
within KKME 1-14 supports the findings from hole KKME 1-6 (located
over 20km away) and further demonstrates there is potential for
nickel enrichment in the magmatic intrusive system. Together with
the encouraging results obtained from hole KKME 1-6, the combined
drill hole findings provide important geological information which
will help plan a Phase II drill programme which aims to vector
towards significant quantities of magmatic nickel-copper
mineralisation within this fertile magmatic system.
KKME 1-14 was drilled targeting a broad kilometre-scale EM
anomaly which can be traced further to the east, which is the known
orientation of magmatic layering within the MFC. This same EM
anomaly extends towards the west and then swings southwest into the
northeast-southwest trending sheer zone which is interpreted to
represent a feeder zone on the Project. As a result, Kalahari Key
is of the belief that this conductive target potentially represents
a much larger Ni-Cu mineralised system than originally
understood.
NEXT EXPLORATION STEPS:
Technical work is continuing including further core inspection
of the third drill hole K1-11a and assay testing of samples from
this hole together with assay testing of additional samples from
K1-6 where further sulphides have been identified.
A further update will be provided in due course summarising all
the technical work completed.
Notably, the technical work includes planning a Phase II
drilling programme which is being designed to intersect the up-dip
part of the mineralised pyroxenites identified in KKME 1-6, as well
as where the east-west oriented EM anomaly intersects the magmatic
feeder zone. Further information in respect of this work and
associated exploration plans will be provided in due course.
Assaying Technique and Results
Scientific Services Geological Laboratories ("SCISERV") located
in Cape Town, South Africa, analysed half core samples for nickel,
copper, gold and platinum with the results summarised in Table 1
and 2 below.
SCISERV employed a two acid (HNO(3) + HF) digest with analysis
by inductively coupled plasma optical emission spectrometry
("ICP-OES").
Table 1: Diamond Drill Hole KKME 1-6 Assay Data
Drill From To (m) Downhole Cu (ppm) Ni (ppm) Zn (ppm) Au (g/t) Pt (g/t)
Hole (m) Interval
ID (m)
1-6 292.68 293.40 0.72 <5 1417 50 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 293.40 294.18 0.78 <5 1213 57 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 294.18 294.70 0.52 6 1177 59 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 294.70 295.28 0.58 163 6606 95 0.05 0.19
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 295.28 295.96 0.68 60 1182 55 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 295.96 296.47 0.51 <5 1235 54 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 296.47 297.48 1.01 15 1621 57 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 296.94 297.48 0.54 <5 2244 69 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 308.49 309.04 0.55 17 1779 63 <0.05 0.11
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 309.04 309.61 0.57 159 3280 73 <0.05 0.08
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 309.61 310.05 0.44 664 6999 79 <0.05 0.15
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 310.05 310.67 0.62 530 7018 80 <0.05 0.15
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 310.67 311.22 0.55 448 7459 82 <0.05 0.15
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 311.22 311.58 0.36 343 4867 77 <0.05 0.13
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 311.58 312.00 0.42 185 4065 63 0.05 0.10
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 312.00 312.41 0.41 35 3714 63 <0.05 0.10
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 312.41 313.19 0.78 21 2558 54 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 501.80 502.98 1.18 <5 1212 57 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 502.98 503.55 0.57 <5 1076 63 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 503.55 504.50 0.95 <5 1237 58 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 504.50 505.40 0.90 <5 1501 53 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 505.40 506.23 0.83 <5 1088 58 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 506.23 507.15 0.92 <5 1140 62 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 507.15 508.00 0.85 <5 1411 63 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 508.00 509.00 1.00 7 1883 57 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 509.00 510.00 1.00 8 1974 51 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 510.00 511.00 1.00 6 1953 57 <0.05 0.06
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 511.00 512.00 1.00 8 1888 56 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 512.00 513.00 1.00 7 2081 57 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 513.00 514.00 1.00 9 1862 55 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 514.00 514.50 0.50 7 2131 65 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 514.50 516.00 1.50 8 1934 55 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 516.00 517.00 1.00 7 1269 42 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 517.00 518.52 1.52 <5 1414 53 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 518.15 518.52 0.37 <5 1489 50 0.208 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 518.52 519.47 0.95 <5 1047 63 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 519.47 520.28 0.81 <5 1740 54 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 520.28 521.22 0.94 <5 1692 53 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 521.22 521.78 0.56 <5 1629 61 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 521.78 522.62 0.84 <5 1606 54 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 522.62 523.13 0.51 <5 1504 64 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 523.13 524.00 0.87 <5 1467 63 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 524.00 524.48 0.48 <5 1642 59 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 524.48 525.28 0.80 <5 1239 60 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 525.28 526.20 0.92 <5 924 63 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 526.20 527.46 1.26 <5 698 51 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 527.46 528.17 0.71 <5 911 58 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 528.17 529.05 0.88 <5 918 65 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 585.00 586.00 1.00 <5 2536 47 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 594.40 595.17 0.77 <5 2469 45 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 595.17 596.00 0.83 <5 2755 47 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 596.00 597.00 1.00 5 3038 52 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
1-6 597.00 597.80 0.80 6 2852 53 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ---------
Table 2: Diamond Drill Hole KKME 1-14 Assay Data
Drill From To (m) Downhole Ni (ppm) Cu (ppm) Au (ppm) Pt (ppm) Notes
Hole (m) Interval
ID (m)
Composite
6.0m @
0.17% Ni
from 180.0m
in harzburgite
rock immediately
above a
fault zone
1-14 180.00 181.00 1.00 1,785 <5 <0.05 <0.05 at 186m
------- ------- ---------- --------- --------- --------- --------- ------------------
1-14 181.00 182.00 1.00 1,821 <5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ------------------
1-14 182.00 183.00 1.00 1,653 <5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 183.00 184.00 1.00 1,914 <5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 184.00 185.00 1.00 1,609 <5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 185.00 186.00 1.00 1,569 <5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- --------- ------------------
1.0m @
0.11% Ni
from 194.0m
in serpentinite
with a
partial
breccia
texture
within
an intra-fault
zone totalling
9m @ 0.07%Ni
between
192m and
1-14 188.16 188.80 0.64 501 138 <0.05 <0.05 201m downhole.
------- ------- ---------- --------- --------- --------- ---------
1-14 192.20 193.00 0.80 708 9 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 193.00 194.00 1.00 779 9 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 194.00 195.00 1.00 1,135 16 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 195.00 196.00 1.00 812 14 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 196.00 197.00 1.00 899 17 0.06 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 197.00 198.00 1.00 659 12 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 198.00 199.00 1.00 705 14 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 199.00 199.65 0.65 826 14 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 199.65 200.40 0.75 566 53 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 200.40 201.20 0.80 128 25 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 207.90 208.50 0.60 6 <5 0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 475.40 476.09 0.69 6 11 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 476.09 477.00 0.91 <5 <5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 477.00 477.90 0.90 <5 <5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 477.90 478.65 0.75 6 <5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 478.65 479.57 0.92 15 9 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 479.57 480.17 0.60 61 106 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 480.17 481.00 0.83 60 56 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 481.00 481.48 0.48 19 5 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 481.48 482.40 0.92 71 48 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
1-14 482.40 483.22 0.82 103 71 <0.05 <0.05
------- ------- ---------- --------- --------- --------- ---------
Further Details
Hole KKME 1-14 was drilled at an azimuth of 345deg with a dip of
60deg to a final depth of 515.8m. The hole was designed to
intercept a conductive body modelled from ground-based TDEM
geophysical survey which was expected to lie at roughly 500m
down-hole depth. The cause of this prospective conductor is still
unknown.
Drill hole KKME 1-11a, the third and final hole of the
proof-of-concept drill programme, is located in the Project's Chipo
(Gift) Northern Target Area, 1,250m west of 1-14.
References:
1: Significant Ni intersections derived from weighted averages
of samples intervals above a nominal 0.13%Ni. Figures are rounded.
10,000ppm = 1%.
2: Assay results for diamond drill hole KKME 1-6 were announced
8 April 2021.
Feeder zone The plumbing system from which magma is supplied
into the intrusive from the lower crust. These can often form as
elongated dykes at the base of an ultramafic layered intrusion.
Sulphide mineral accumulations can often form in the vicinity of
the feeder zone.
Harzburgite Harzburgite is a type of peridotite ultramafic
igneous rock, with no or very little monoclinic pyroxene and
consisting only of olivine and orthorhombic pyroxene bronzite.
Harzburgite typically forms by the extraction of partial melts from
the more pyroxene-rich peridotite.
Serpentinite A metamorphic rock formed as a result of the low
temperature anaerobic oxidation of ultramafic rock in the course of
which density is reduced and volume increased by the addition of
water, and nickel and other elements undergo remobilisation as a
result of hydrothermal activity.
Ultramafic rock An igneous rock in which has a very low silica
content and in which more than 90% of the rock is composed of
magnesium and iron-rich minerals like pyroxenes, amphiboles, and
olivine.
COMPETENT PERSON STATEMENT
The drilling and sampling programme has been overseen on site by
Mr. Ian McGeorge MSc CGeol FGS a qualified person and chartered
geologist working on behalf of the independent mining consultancy
The MSA Group ("MSA"). Information in this announcement relating to
the exploration drilling results is based on data reviewed by Mr
McGeorge. Mr McGeorge has sufficient experience 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 under the AIM Rules - Note for Mining and Oil
& Gas Companies. Mr McGeorge consents to the inclusion of the
exploration results in the form and context in which they
appear.
The technical information contained in this disclosure has been
read and approved by Mr Nick O'Reilly (MSc, DIC, MIMMM, MAusIMM,
FGS), who is a qualified geologist and acts as the Competent 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.
This announcement contains inside information for the purposes
of Article 7 of the Market Abuse Regulation (EU) 596/2014 as it
forms part of UK domestic law by virtue of the European Union
(Withdrawal) Act 2018 ("MAR"), and is disclosed in accordance with
the Company's obligations under Article 17 of MAR.
For further information please visit
https://www.powermetalresources.com/ or contact:
Power Metal Resources plc
Paul Johnson (Chief Executive Officer) +44 (0) 7766 465 617
SP Angel Corporate Finance (Nomad and Joint Broker)
Ewan Leggat/Charlie Bouverat +44 (0) 20 3470 0470
SI Capital Limited (Joint Broker)
Nick Emerson +44 (0) 1483 413 500
First Equity Limited (Joint Broker)
David Cockbill/Jason Robertson +44 (0) 20 7330 1883
Notes to Editors:
Power Metal Resources plc (LON:POW) is an AIM listed metals
exploration and development company seeking large scale metal
discoveries
The Company has a global portfolio of project interests
including precious, base and strategic metal exploration in North
America, Africa and Australia. Project interests range from early
stage greenfield exploration to later stage exploration prospects
subject to drill programmes.
The Board and its team of advisors have expertise in project
generation, exploration and development and have identified an
opportunity to utilise the Company's position to become a leader in
the London market for investors wishing to gain exposure to
proactive global metals exploration.
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