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2020 Diamond Drill Program Highlights:
- Positive results in identifying polymetallic anomalous values
for gold, silver, nickel, zinc and chromium
- Future drill programs will target potential higher-grade
polymetallic mineralization at Western Atlas' district scale
Meadowbank project
- First drill program ever on these properties consisted of 13
drill holes for a total of 3,545 meters drilled in Target B1, Block
B, south of Agnico Eagle's Meadowbank mine and contiguous to Agnico
Eagle's Greyhound project
- The 2020 drill program targeted banded iron formation (BIF) and
shear zones, confirms geological settings and conditions favourable
for the development of orogenic gold deposits in the area and
highlights anomalous values for nickel, and chromium. Anomalous
gold, nickel, chromium and zinc intersections includes (see also
Table1):
-
- WA20-003 intercepted 0.30 m at
1.27 g/t Au and 12.30 g/t Ag from 253.23
m, and 0.77 m at 0.15% Zn from
245.08 m (Zone 1);
- WA20-013 intercepted 0.45 m at
1.39 g/t Au from 5.20 m, 7.38 m at 0.12% Ni and 0.21% Cr from 142.42 m and 9.33 m
at 0.14% Ni and 0.21% Cr from 177.70
m (Zone 2);
- WA20-004 intercepted 7.75 m at
0.12% Ni and 0.21% Cr from 102.15 m
(Zone 2);
- WA20-005 intercepted 8.45 m at
0.15% Ni and 0.25% Cr from 85.40 m
(Zone 2);
- WA20-006 intercepted 11.60 m at
0.10% Ni and 0.25% Cr from 205.23 m
and 2.23 m at 0.12% Ni and 0.27% Cr
from 239.66 m and 2.75 m at 0.10% Ni and 0.22% Cr from 249.15 m (Zone 2);
- WA20-011 intercepted 2.98 m at
0.15% Ni and 0.22% Cr from 119.75 m
(Zone 5);
- Target B1 is only one of six targets for follow up with
drilling so far identified within Blocks A and B
-
- Drilling of Block A, North of Block B and located between
Agnico Eagle's Meadowbank and Amaruq, is being planned for next
drill program.
VANCOUVER, BC, Nov. 30, 2020 /CNW/ - Western Atlas
Resources Inc. ("Western Atlas" or the "Company")
(TSXV: WA), announces results from the diamond drill program
conducted at its Meadowbank Project located in Nunavut, Canada. The 13 hole drill program
targeted banded iron formation (BIF) and shear zones within Target
B1, Block B (Table 2 and Figure 3). Target B1 is one of the six
targets for follow up and drilling identified within Blocks A and B
(Figures 1 and 2). The 2020 drill program is the first of several
drill programs the Company intends to undertake in order to test
these targets.
Summary
The program intersected elevated gold assays in quartz-carbonate
vein breccias within the shear zone in Zone 1. Two vein breccia
intervals were intersected in hole WA20-001. Gold mineralization
extends into the network of quartz-carbonate veins and veinlets
also enriched in silver and zinc in hole WA20-003. Associated with
the anomalous gold assays are occurrences of coarse arsenopyrite
and pyrite in veins/veinlets and intense ankerite-grunerite
alteration haloes along the veins.
In Zone 2 anomalous gold and silver were intersected in a
quartz-carbonate vein within BIF trending to northeast and parallel
to the main BIF zone approximately 180m to the south. Anomalous chromium and nickel
assays were encountered in serpentinized fine-grained and
komatiitic ultramafics.
Gold values similar to those encountered in Zone 1 were
encountered in Zone 3. Mineralization occurs in quartz veins and
veinlets in three BIF layers intersected there. Associated with
anomalous gold assays is 1-5% pyrite and strong ankerite alteration
(for more details please refer to Drill Hole Review to this
press release).
Summary of Anomalous Results:
HOLE
NUMBER
|
TARGET
|
FROM
(m)
|
TO
(m)
|
LENGTH
(m)
|
Au
g/t
|
Ag
g/t
|
Ni%
|
Cr%
|
WA20-003
|
ZONE
1
|
253.23
|
253.53
|
0.30
|
1.27
|
12.3
|
|
|
WA20-013
|
ZONE
2
|
5.20
|
5.65
|
0.45
|
1.39
|
|
|
|
WA20-013
|
ZONE
2
|
142.42
|
149.80
|
7.38
|
|
|
0.12
|
0.21
|
WA20-013
|
ZONE
2
|
177.70
|
187.03
|
9.33
|
|
|
0.14
|
0.21
|
WA20-004
|
ZONE
2
|
102.15
|
109.90
|
7.75
|
|
|
0.12
|
0.21
|
WA20-005
|
ZONE
2
|
85.40
|
93.85
|
8.45
|
|
|
0.15
|
0.25
|
WA20-006
|
ZONE
2
|
205.23
|
216.83
|
11.60
|
|
|
0.10
|
0.25
|
WA20-006
|
ZONE
2
|
239.66
|
241.89
|
2.23
|
|
|
0.12
|
0.27
|
WA20-006
|
ZONE
2
|
249.15
|
251.90
|
2.75
|
|
|
0.10
|
0.22
|
WA20-011
|
ZONE
5
|
119.75
|
122.73
|
2.98
|
|
|
0.15
|
0.22
|
Table 1: Anomalous results
Fabio Capponi, CEO stated: "We
are excited by the results of this reconnaissance drill program,
the first ever to be drilled on Western Atlas's 580km2
Meadowbank mineral properties. We have demonstrated favourable
geological settings for gold and silver mineralization as well as
for nickel and other base metals. Future systematic drill programs
will aim at testing potential higher grade mineralization of gold,
silver and these base metals within the six targets so far
identified within Block A and B."
The definition of these drill targets is the result of the
initial interpretation of the 2017 to 2019 exploration program data
sets, which include detailed field mapping and sampling program
(yielded gold including 13.30 g/t Au and up to 44.7 g/t Ag), over
3,800 km of airborne magnetic survey, over 1,500 line-km of
helicopter-borne VTEM followed by electromagnetic (EM) anomaly and
airborne inductive induced polarization (AIIP) processing report,
over 32 line-km of ground induced polarization (IP) survey over
specific targets.
Drillholes were designed to test both geophysical targets and
favorable geological features (BIF and shear zones) in five
separate areas referred to as Zones 1 to 5 in Target B1. Holes
drilled in Zone 1 and Zone 3 also tested locations of grab samples
with anomalous gold values collected during the 2018 mapping and
prospecting program.
Regional and local geological settings, structures, metamorphic
grade, mineralization and alteration patterns encountered during
the 2020 exploration program indicate conditions favourable for the
development of orogenic gold deposits in the area and highlights
anomalous values for nickel, zinc and chromium.
Similarities between the geology and mineralization of Agnico's
Meadowbank and Amaruq mines and that of Target B1 geology
include:
- Algoma-type BIF in combination with ultramafic rocks similar to
that present in Agnico's Goose and Portage deposits (part of
Agnico's Meadowbank mine) have been encountered in Zones 2 and
4
- Amaruq volcanic and fine-grained sediment sequences are similar
to volcanic-sedimentary sequence in Zone 2
- Ultramafic volcanic rocks at Agnico Eagle's Amaruq and
Meadowbank deposits similar to that encountered within Target B1
are associated with gold hosting sulphide mineralization
- Pyrite and pyrite-pyrrhotite mineralization in clastic
sediments in Zone 2 are equivalent to stratiform sulphide
mineralization encountered in Amaruq.
Hole #
|
Hole-ID
|
Area
|
Platform
|
Azimuth
[*]
|
Dip
[*]
|
Total Depth
(m)
|
Collar Easting
(NAD83, UTM
Zone 14)
|
Collar Northing
(NAD83, UTM
Zone 14)
|
Collar Elevation
(Meters Above
Sea Level)
|
1
|
WA20-001
|
Zone 1
|
WA1
|
345
|
-50
|
347.42
|
641705.8
|
7178358.6
|
99.8
|
2
|
WA20-002
|
Zone 1
|
WA1A
|
312
|
-50
|
321.00
|
641546.0
|
7178399.2
|
101.2
|
3
|
WA20-003
|
Zone 1
|
WA1
|
325
|
-50
|
315.00
|
641705.8
|
7178358.6
|
99.8
|
4
|
WA20-004
|
Zone 2
|
WA2
|
340
|
-60
|
252.00
|
642523.6
|
7179903.6
|
106.4
|
5
|
WA20-005
|
Zone 2
|
WA2
|
340
|
-50
|
171.00
|
642523.6
|
7179903.6
|
106.4
|
6
|
WA20-006
|
Zone 2
|
WA2A
|
340
|
-50
|
288.00
|
642724.4
|
7179889.9
|
93.7
|
7
|
WA20-007
|
Zone 3
|
WA3
|
340
|
-50
|
255.00
|
636266.1
|
7178917.7
|
108.3
|
8
|
WA20-008
|
Zone 3
|
WA3
|
340
|
-60
|
180.00
|
636266.1
|
7178917.7
|
108.3
|
9
|
WA20-009
|
Zone 4
|
WA4
|
340
|
-50
|
282.00
|
637797.8
|
7177444.2
|
107.0
|
10
|
WA20-010
|
Zone 4
|
WA4
|
340
|
-60
|
267.00
|
637797.8
|
7177444.2
|
107.0
|
11
|
WA20-011
|
Zone 5
|
WA5
|
340
|
-50
|
273.00
|
639457.4
|
7178119.5
|
98.6
|
12
|
WA20-012
|
Zone 1
|
WA1B
|
345
|
-50
|
294.00
|
641724.5
|
7178393.6
|
100.1
|
13
|
WA20-013
|
Zone 2
|
WA2B
|
340
|
-50
|
300.00
|
642677.1
|
7179916.0
|
97.1
|
Total Drilled
[m]
|
3,545.42
|
|
Table 2: Drillholes details
Drill Hole Review:
All intervals referred to herein are core lengths. Insufficient
drilling has been completed to estimate true widths.
Zone 1
Four holes (WA20-001, -002, - 003 and -012) were drilled
north-northwest or northwest into the shear zone covered by a
50 m to 60
m wide swampy area. BIF lense parallel to the shear zone
outcrops south of the shear zone. A grab sample collected from the
BIF during the 2018 mapping program, assayed 13.3 g/t Au.
Within the shear zone, the holes intersected mafic volcanics,
laminated felsic volcanics/sediments and ultramafics. Lithologies
within the shear zone are intensely carbonatized and locally
silicified. Mafic and felsic volcanics are ankerite and grunerite
altered, and ultramafics are flooded and veined with carbonates.
Pyrite-arsenopyrite mineralization is associated with ankerite
alteration and quartz-carbonate veining. Pyrrhotite mineralization
is associated with silicified intervals.
In hole WA20-001, two quartz-carbonate vein breccia intervals
were intersected from 221.08 m to
224.17 m (3.09
m) and from 251.63 m to
254.79 m (3.36
m). These intervals contained from 1 to 5% pyrite and minor
arsenopyrite. Minor arsenopyrite was also intersected over narrow
intervals in holes WA20-003 and WA20-012. Auriferous arsenopyrite
is one of the ore minerals in Amaruq.
Anomalous intersections from Zone 1 include 0.72 m grading 0.12g/t Au from 222.78 m to 223.50
m; 0.55 m grading 0.14g/t Au
from 224.17 m to 224.72 m and 1.40m
grading 0.18 g/t Au from 252.80 m to
254.20 m in hole WA20-001. Hole
WA20-002 intersected 0.50 m grading
0.24g/t Au from 138.05 m to
138.55 m. Approximately 50 m to the west, 0.34
m grading 0.23g/t Au from 247.77 m to 248.11
m and 2.11 m grading 0.28g/t
Au from 251.42 m to
253.53 m were intersected in hole
WA20-003. This interval includes 0.30
m grading 1.27g/t Au and 12.3 g/t Ag from 253.23 m to 253.53
m. 0.77m grading 0.15% Zn from
245.08 to 245.85 were also intersected in hole WA20-003.
Zone 2
Four holes (WA-004, -005, -006, and -013) tested the Zone 2
which is dominantly underlain by a volcanic-sedimentary assemblage
composed of komatiitic flows, massive ultramafic volcaniclastics
and intercalated fine-grained clastic sediments (argillites and
siltstones), overlain by a BIF sequence over 100 m in thickness. Sediments within this
assemblage, particularly argillite layers, host pyrite
mineralization. Argillites at the contact with BIF are consistently
mineralized with pyrrhotite and pyrite.
This mineralized zone with 3-10% vol sulphides is 19.12 m wide in hole WA20-006 (core length). The
westernmost hole in Zone 2, WA20-006, intersected this style of
mineralization with 3% to 10% pyrite-pyrrhotite from 264.73 m to 283.85
m (19.12 m) and the
easternmost hole, WA20-004, intersected 5% to 10% pyrite-pyrrhotite
from 127.80 m to 135.15 m (7.38
m).
The mineralized zone has been intersected along the strike over
210m and is open along strike and at
depth.
- Chromium and nickel in serpentinized ultramafic flows were
intersected in holes WA20-004, WA20-005, WA20-006 and WA20-013.
Hole WA20-004 intersected 7.75m
grading 0.12% Ni and 0.21% Cr from 102.15
m to 109.90 m. The interval
includes 3.14m grading 0.17% Ni and
0.29% Cr from 104.18 m to
107.32 m. Hole WA20-005 intercepted
8.45 m grading 0.15% Ni and 0.25% Cr
from 85.40 m to 93.85 m. Hole WA20-006 intercepted 11.60 m grading 0.10% Ni and 0.25% Cr from
205.23 m to 216.83 m, 2.23 m
grading 0.12% Ni and 0.27% Cr from 239.66
m to 241.89 m and 2.75 m grading 0.10% Ni and 0.22% Cr from
249.15 m to 251.90 m. Hole WA20-013 intersected 7.38m grading 0.12% Ni and 0.21% Cr from
142.42 m to 149.80 m and 9.33m
grading 0.14% Ni and 0.21% Cr from 177.70
m to 187.03 m.
In Zone 2, anomalous gold was intersected in hole WA20-013 in a
quartz-carbonate vein cutting BIF at 5.20
m to 5.65 m (0.45 m core length) which assayed 1.39g/t Au.
Zone 3
Two drill holes drilled in Zone 3 (WA20-007, -008) were designed
to test airborne magnetometry and ground IP geophysical anomaly in
the area of a grab sample which assayed 6.89 g/t Au in 2018. Both
holes intersected Amarulik formation greywackes and three narrow
BIF intervals.; BIF intervals are ankerite altered, with magnetite
mostly destroyed. Fine-grained crystalline pyrite forms 1-3% volume
in BIF layers, except for the BIF layer in hole WA20-008 from
52.42 m to 53.40 m (0.98m core
length) in which pyrite forms 5 to10% volume.
Hole WA20-007 intersected 0.38 m
grading 0.13g/t Au from 47.47 m to
47.85 m in the southern BIF layer.
The same layer assayed 0.23g/t Au over 0.98
m in hole WA20-008 from 52.42
m to 53.40 m.
The middle BIF layer assayed 0.11g/t Au over 0.48 m in hole WA20-007 from 85.98 m to 86.46 m
and 0.20g/t Au over 0.83 m in hole
WA20-008 from 88.03 m to 88.86 m.
Northern layer was intersected in hole WA20-008 from
144.52 m to 145.08 m and it assayed 0.38g/t Au over
0.56 m.
Zone 4
Two drill holes collared from the platform WA4 (WA20-009, -010)
were drilled to test a low resistivity and high chargeability
geophysical target associated with BIF and shear zone. Both
holes intersected porphyritic dacite flow between the felsic
volcaniclastics and BIF. The BIF lens is 50m wide (true width) and similar to BIF in Zone
WA2. At the northern BIF contact, a 25
m wide shear zone composed of fault vein breccia intervals
and sheared mafic volcanic, argillite and siltstone intervals
occur.
The shear zone north of the BIF was intersected over
28.72 m in hole WA20-009 (from
206.15 m to 234.8 7 m), while in hole WA20-010 the shear zone is
32.47 m wide (from 228.35 m to 260.82
m). Mineralization is associated with mafic volcanics and
graphitic argillites. Mineralization in veins varies, within the
BIF and in the siltstone intersected in hole WA20-009
mineralization is weaker (four intervals from 1.5 m to– 2 m wide
with approximately 5% pyrite in hole WA20-009). In hole WA20-010,
mafic volcanics dominate the shear zone and mineralization is more
continuous. The interval from 231.03
m to 252.00 m contains an
average of 5% pyrite (20.97 m core
length) including pyrite content over 10% from 247.26 m to 249.15 (1.89
m core length).
No anomalous gold intersections.
Zone 5
One drill hole (WA20-011) was designed to test a low resistivity
and high chargeability geophysical target associated with shear
zones and BIFs. It intersected 120 m
of ultramafic volcanics intercalated between intermediate or mafic
volcanics to the south and intermediate volcanics to the north.
Within the ultramafic assemblage is an 8.50m thick chert interval.
From 107.31 m to 119.75 m, a 12.44 m
interval along the chert layer is locally mineralized with pyrite
varying between 3% and 10%. Hole WA20-011 intercepted 2.98 m grading 0.15% Ni and 0.22% Cr from
119.75 m.
QA / QC Protocols
Individual drill core samples were sawn in half, labeled, placed
in plastic sample bags, and sealed. The remaining drill core is
securely stored in Baker Lake.
Groups of samples were placed in bags sealed with uniquely numbered
security tags and shipped directly to Activation Laboratories Ltd.
("Actlabs") in Ancaster, Ontario
for analysis. The Actlabs facility is accredited to ISO 17025:2017
standards and to the Standards Council of Canada (SCC) Requirements and Guidance for the
Accreditation of Testing Laboratories.
Samples were weighed then crushed to a nominal 2 mm,
mechanically split to obtain a representative sample (250 g) and
then pulverized to at least 95% passing 105 microns (μm).
Multi-element analysis package determined 38 elements including
copper, zinc, lead and silver assays were determined by Aqua Regia
digestion with ICP-OES finish. Gold (30g sample of the pulverized
material) was analyzed by fire assay fusion with AAS finish.
Company QA/QC included the insertion and continual monitoring of
standards, blanks, and duplicates.
Paul Chamois, P.Geo, is the Qualified Person as defined by
National Instrument 43-101 and is responsible for reviewing and
supervising the preparation of the scientific and technical
disclosure in this news release.
About Western Atlas
The Company's common shares are listed on the TSX Venture
Exchange under the symbol WA. Western Atlas is focused on the
acquisition and development of scalable precious metals projects in
premier mining jurisdictions. Western Atlas's wholly owned
subsidiary, 5530 Nunavut Inc., holds its interests in the
Meadowbank project located in Nunavut,
Canada.
Cautionary Statement Regarding Forward-Looking
Information
This news release includes certain "forward-looking statements"
under applicable Canadian securities legislation that are not
historical facts. Forward-looking statements involve risks,
uncertainties, and other factors that could cause actual results,
performance, prospects, and opportunities to differ materially from
those expressed or implied by such forward-looking statements.
Forward-looking statements in this news release include, but are
not limited to, statements with respect to the Company's
objectives, goals or future plans; the receipt of the requisite
approvals with respect to the business and operations of the
Company. Forward-looking statements are necessarily based on a
number of estimates and assumptions that, while considered
reasonable, are subject to known and unknown risks, uncertainties
and other factors which may cause actual results and future events
to differ materially from those expressed or implied by such
forward-looking statements. Such factors include, but are not
limited to: general business, economic and social uncertainties;
litigation, legislative, environmental and other judicial,
regulatory, political and competitive developments; delay or
failure to receive board, shareholder or regulatory approvals;
those additional risks set out in Western Atlas's public documents
filed on SEDAR at www.sedar.com; and other matters discussed in
this news release. Although Western Atlas believes that the
assumptions and factors used in preparing the forward-looking
statements are reasonable, undue reliance should not be placed on
these statements, which only apply as of the date of this news
release, and no assurance can be given that such events will occur
in the disclosed time frames or at all. Except where required by
law, Western Atlas disclaims any intention or obligation to update
or revise any forward-looking statement, whether as a result of new
information, future events, or otherwise.
Reader Advisory Neither the TSX Venture Exchange nor
its Regulation Services Provider (as that term is defined in the
policies of the TSX Venture Exchange) accepts responsibility for
the adequacy or accuracy of this release.
SOURCE Western Atlas Resources