5 March 2024
BWA
Group PLC
("BWA", or
the "Company") (AQSE: BWAP)
Reconnaissance
Site Visit to the Isoukustouc Licence, Kings of the North Project,
Quebec, Canada
Board
Refocus - Change of Roles
BWA Group
plc [AQSE: BWAP], which has mineral exploration licences in both
Cameroon and Canada and is quoted on London's AQSE Growth Market, provides an
update on its recently completed reconnaissance site visit to
the Isoukustouc
licence group, Quebec, Canada
("Isoukustouc"
or "Isoukustouc
Project"),
held by the Company's wholly owned subsidiary, Kings of the North
Corp. ("KOTN"),
as well as a revision of Board roles..
Reconnaissance
Site Visit to the Isoukustouc Licence
The
Isoukustouc licence group is in the North-Shore region of the
St-Lawrence River, in proximity to the communities of Baie Comeau (80 km south) and Sept-Îles (150
km east). The Isoukustouc licence is located less than ten
kilometres to the northeast of the Manic-3 hydro generating station
within the Manicouagan Reservoir. The Isoukustouc licence consists
of 30 claims totalling 16.5 km2.
The
licence area is prospective for intrusion-related Ni-Cu(-PGE)
sulphide mineralisation, with a recent potential addition of
magmatic lithium. Several Ni-Cu-PGE occurrences have been uncovered
recently in the Grenville
Province, including the Cu-Ni mineralisation associated with
mafic intrusions of the Lac Volant Occurrence in the Matamec
Complex.
A version
of this announcement including maps and photographs can be viewed
on the Company's website, http://www.bwagroupplc.com/bwa-announcements.html
Summary
A four-day
initial prospecting site visit to the KOTN Isoukustouc licence was
completed, during which ten surface samples were taken from
accessible areas near geophysical anomalies from the recently
completed Rio Tinto VTEM surveys.
The visit
was conducted to inspect the terrain, and `ground truth' general
geology, collect preliminary samples across existing known targets
and some recently identified geophysical anomalies, and gain a
better understanding of the site's access and general site
understanding and infrastructure of the project area.
Three
known prospects exist from previous exploration, namely Manic-3
(Lac Louise), B-40 and Mathilda, where disseminated and massive
sulphides are associated with magmatic rocks of Gabbroic
composition.
The
sulphides encountered consist of pyrite, pyrrhotite, chalcopyrite
and pentlandite.
One
occurrence contains nickel, copper and platinum group elements
("PGE")
mineralisation related to mafic and ultramafic rocks.
A total of
ten samples were collected over the site visit and were shipped to
ALS Loughrea for analysis.
Further
details can be found below.
James Butterfield, Managing Director of BWA,
commented:
"We
are pleased to have conducted a preliminary albeit limited site
visit to Isoukustouc and are extremely encouraged with the
anomalous levels of mineralisation that have been received. Results
show that the area is prospective as thought and BWA look forward
to defining a more comprehensive study plan and exploring the
licence in a more systematic and thorough manner in the near
future."
Board
Refocus
Given the
number of board changes at BWA over the last 6 months, it has taken
a while for matters to settle down, be it the day-to-day management
of the group or shaping its strategy for the immediate and
medium-term future. And since working together for a period of time
now, individual's strengths have come to the fore. As result it has
been decided, in consultation with our Advisers, including Allenby
Capital, that the following board changes should be
made:
-
Chairman -
Jonathan Wearing
-
To focus
on BWA's strategy and City liaison matters.
-
Managing
Director - James
Butterfield
-
With in
depth knowledge of the Group, he will take up the role of Managing
Director to concentrate on the group's day-to-day
activities.
-
Director -
John Byfield
-
Will
continue in his role as the `Independent Director'
within
BWA and to
focus on the Group's legal and corporate matters.
These
changes will take effect from 1 April
2024.
For
further information on the Company, please visit:
http://www.bwagroupplc.com/index.html
or
contact:
BWA
Group PLC
James
Butterfield
Managing
Director
|
+44 (0)
7770 225 253
enquiries@bwagroupplc.com
|
Allenby
Capital Limited
Corporate
Adviser
Nick
Harris/Lauren Wright
|
+44 (0)20
3328 5656
|
Additional Information on the Reconnaissance Site Visit
to the Isoukustouc Licence, Kings of the North Project,
Quebec,
Canada
Sample
Results
From the
limited number of widespread rock grab samples taken during the
prospecting site visit two samples located near one of the
geophysical anomalies and near historic drillhole 50596 (no assays
found) at Manic-3 returned anomalous copper and nickel values with
associated anomalous cobalt and magnesium, with one sample also
returning anomalous silver (AMS132 and AMS130). A third sample
taken at Manic-3 returned elevated strontium with above background
nickel (AMS 128).
Results of
key target and anomalous elements are presented below.
Three
samples taken from the B-40 S location (AMS134, 135, 136) and close
to the margin of a moderate geophysical anomaly (conducted by
Geotech for Rio Tinto) returned elevated values for strontium and
titanium. No significant elevated gold results were observed in the
samples collected.
Sample
No
|
East
|
North
|
Prospect
|
Lithology
|
ICP61
Ag_ppm
|
ICP61
Co_ppm
|
ICP61
Cu_ppm
|
ICP61
Mg_%
|
ICP61
Ni_ppm
|
ICP61
Pb_ppm
|
ICP61
Sr_ppm
|
ICP61
Ti_%
|
ICP61
Zn_ppm
|
AA23
Au_ppm
|
AMS128
|
538089
|
5530871
|
Manic-3
|
Gabbro
|
<0.5
|
41
|
52
|
3.63
|
138
|
5
|
1405
|
0.54
|
86
|
<0.00
|
AMS129
|
537614
|
5531028
|
Manic-3
|
Gabbro
|
<0.5
|
26
|
35
|
2.46
|
34
|
3
|
358
|
0.55
|
127
|
<0.00
|
AMS130
|
537574
|
5531067
|
Manic-3
|
Gabbro
|
<0.5
|
127
|
702
|
11.95
|
1090
|
2
|
151
|
0.3
|
77
|
0.012
|
AMS131
|
537691
|
5531049
|
Manic-3
|
Gabbro
|
<0.5
|
46
|
72
|
4.86
|
73
|
2
|
308
|
0.27
|
132
|
<0.00
|
AMS132
|
537696
|
5531067
|
Manic-3
|
Gabbro
|
2.2
|
109
|
2670
|
5.04
|
427
|
12
|
229
|
0.29
|
146
|
0.058
|
AMS133
|
542364
|
5530177
|
B-40
|
Granite
|
<0.5
|
13
|
7
|
1.44
|
20
|
3
|
447
|
0.2
|
62
|
<0.00
|
AMS134
|
542295
|
5529621
|
B-40
S
|
Gabbro
|
<0.5
|
33
|
71
|
2.19
|
40
|
14
|
2500
|
2.01
|
146
|
<0.00
|
AMS135
|
542240
|
5529561
|
B-40
S
|
Gabbro
|
<0.5
|
55
|
15
|
4.29
|
140
|
<2
|
647
|
1.18
|
99
|
<0.00
|
AMS136
|
542238
|
5529503
|
B-40
S
|
Gabbro
|
<0.5
|
59
|
30
|
4.52
|
150
|
2
|
793
|
1.32
|
102
|
<0.00
|
AMS137
|
538517
|
5525891
|
Mathilda
NE
|
Granite
|
<0.5
|
20
|
44
|
2.59
|
69
|
19
|
379
|
0.51
|
129
|
<0.00
|
Geology
and Geological Interpretation
The
licence is located within the Grenville Geological Province of the
North Shore region of Quebec. The
Grenville Province extends for
more than 2,000 km in length and skirts the North Shore of the
St-Lawrence River and varies in width between 300 km to 600
km.
The
Grenville Province consists of
high-grade metamorphic terrains exposed along the southeastern
margin of the Canadian Shield, which were deformed by the
Grenvillian Orogenic Cycle between 1,160 Ma and 950 Ma. The
tectonic fabric of Grenville is
predominantly northeast-southwest trending. The present-day aspect
of Grenville is the result of a
complex polycyclic structural evolution.
Host
lithologies from the licence belong to the allochthonous polycyclic
belt, composed of paragneisses, orthogneisses, granites, gabbros
and anorthosites. In the licence, metamorphism is a higher grade
from amphibolite to granulite facies. The area is covered by
granite and migmatites of higher metamorphic grade in the upper
amphibolite to granulite facies showing evidence of partial
melting. These rocks have been locally intruded by mafic and
ultramafic rocks such as gabbros, diorites, pyroxenites and
monzonites. The intrusive rocks appear as small plutons and
stocks.
The
mineralisation model type is understood to be an intrusion-related
Ni-Cu(-PGE) disseminated, semi- and massive sulphide, with a recent
potential addition of magmatic intrusion-related
lithium.
Several
nickel-copper-PGE occurrences have been uncovered during the last
few years in the Grenville
Province, including the copper-nickel mineralisation
associated with mafic sills or dykes of the Lac Volant Occurrence
in the Matamec Complex located 35 kilometres north of Lac Méchant.
The known copper-nickel mineralisation (Renzy, Edouard and McNickel
occurrences) are largely lower grade (<1% nickel and <1%
copper). The most significant PGE mineralisation known is
associated with several 2.49 to 2.44 Ga mafic intrusions that
extend from southern Quebec into
Ontario).
Outcropping
mineralisation observed at the Isoukustouc licence occurs as
semi-massive sulphides of pyrrhotite, pyrite (Fe) and potentially
gold (Au) hosting, chalcopyrite (Cu), pentlandite (Ni) and
disseminated sulphides and millimetric stringers observed locally
as a stockwork which is hosted within the gabbros. These intrusive
gabbroic rocks appear from the limited mapping as small plutons or
stocks. Furthermore, these small gabbroic intrusions appear to
coincide with the geophysical anomalies.
Rock types
and alteration/mineralisation observed are largely in line with
expectations from previous studies and reports, indicating most
likely exploration target deposit model type being
intrusion-related sulphides.
However,
the occurrence of other deposit types in old basements and
long-lived terrains such as orogenic base and precious metal
vein/shear type cannot be discounted.
Competent
Person's Statement
The
information in this report which relates to the BWA Isoukustouc
Project is based upon and fairly represents information collected
and compiled by Mr Lewis Harvey,
MSc., Principal Consulting Geologist for Addison Mining Services,
who is a Member of the Australian Institute of
Geoscientists.
The
results were reviewed by Mr J.N.
Hogg, MSc. MAIG, Principal Geologist and CEO for Addison
Mining Services and Non-executive Director of BWAR.
Mr
Harvey and Mr Hogg have sufficient experience relevant to the style
of mineralisation, the type of deposit under consideration and to
the activity undertaken to qualify as a Competent Person as defined
in the JORC Code 2012 edition of the Australasian Code for
Reporting of Exploration Results, Mineral Resources and Ore
Reserves.
Mr
Harvey and Mr Hogg has reviewed and verified the technical
information that forms the basis of and has been used in the
preparation of this announcement, including all sampling and
analytical data, and analytical techniques. Mr Harvey and Mr Hogg
consent to the inclusion in this announcement of the matters based
on the information, in the form and context in which it
appears.
Forward
Looking Statement
This
announcement contains forward-looking statements which involve a
number of risks and uncertainties. These forward-looking statements
are expressed in good faith and believed to have a reasonable
basis. These statements reflect current expectations, intentions or
strategies regarding the future and assumptions based on currently
available information. Should one or more of the risks or
uncertainties materialise, or should underlying assumptions prove
incorrect, actual results may vary from the expectations,
intentions and strategies described in this
announcement.
No
obligation is assumed to update forward-looking statements if these
beliefs, opinions and estimates should change or to reflect other
future developments.
Glossary
of Technical Terms:
"%"
|
percent
|
"AA"
|
Atomic
Absorption
|
"ALS"
|
Australian
Laboratory Services;
|
"AMS"
|
Addison
Mining Services;
|
"BWA"
|
BWA Group
PLC;
|
"CEO"
|
Chief
Executive Officer
|
"CP"
|
Competent
Person;
|
"Ga"
|
Billion
years
|
"km"
|
Kilometre;
|
"KOTN"
|
Kings of
the North
|
"JORC
(2012)"
|
2012
edition of the JORC code;
|
"JORC"
|
Australasian
Code for Reporting of Exploration Results, Mineral Resources and
Ore Reserves, as published by the Joint Ore Reserves Committee of
The Australasian Institute of Mining and Metallurgy, Australian
Institute of Geoscientists and Minerals Council of
Australia;
|
"m"
|
metre;
|
"Ma"
|
Million
years
|
"MAIG"
|
Member of
the Australian Institute of Geoscientists
|
"MSc"
|
Master of
Science
|
"ME-XRF11bE"
|
Analysis
by Fusion/XRF;
|
"PGE"
|
Platinum
Group Elements
|