Fireweed Intersects
4.76%
Zinc,
0.43% Lead and 18.9 g/t Silver
over
43.7
m
in upper sequence and
2.08%
Zinc over
225
m
in
lower sequence
at Boundary West
Vancouver, British Columbia, Canada -- February 25, 2021 --
InvestorsHub NewsWire -- FIREWEED ZINC LTD.
("Fireweed") (TSXV: FWZ) is pleased to announce the
final
results
from
the 2020 drilling at Boundary
Zone, Macmillan Pass
Project in Yukon, Canada. These results
are
from
Boundary Zone West
which
was discovered in
2020 with a
360
metre
step out hole drilled on a
gravity anomaly. It is located 15 road
kilometres west of the Tom-Jason deposits (see Map
1)
and
includes
discovery of a
new lower
sequence hosted in older
host rocks than other mineralization found at Macmillan
Pass.
Boundary Zone has
now been traced over a strike length of 630
metres,
and both upper and lower sequence mineralization remains open for
expansion along strike and
down dip.
Highlights
-
Hole
NB20-009
intersected
a
dense
upper
sequence of
4.76%
zinc,
0.43%
lead
and 18.9
g/t
silver
over 43.7
m
including a high grade
stratiform zone of 26.35%
zinc,
5.21%
lead
and 53.4
g/t
silver
over 2.19
m
from
a
vertical
depth
of 40
m from
surface.
-
Hole
NB20-009 also
intersected
a broad
lower
sequence of
2.08%
zinc
over
225.0
m including a stratiform zone
of 3.69%
zinc
over
19.0 m and a
vein
interval of 3.75% zinc
over
50.00 m.
-
This
is the first
discovery of
zinc mineralization
hosted
by lower
sequence Ordovician-Silurian
rocks in the district.
-
Hole
NB20-008 intersected the upper sequence
of vein mineralization of 2.48% zinc,
0.74% lead, and 12.5
g/t
silver over
111.17
m including two
higher grade vein intervals of 6.07% zinc, 1.12% lead, and
27.8 g/t silver over 13.95 m and 4.57% zinc, 0.62% lead, and
15.2 g/t silver over 17.0 m
Table 1:
Highlight
results
from
the upper and lower sequences at
Boundary Zone
West.
Drill
Hole
|
From (m)
|
To (m)
|
Intersection (m)
|
Zinc (%)
|
Lead (%)
|
Silver (g/t)
|
Bulk Density (t/m3)
|
Zone
|
NB20-008
|
194.83
|
306.00
|
111.17
|
2.48
|
0.74
|
12.5
|
3.37
|
Upp.V
|
>
including
|
198.05
|
212.00
|
13.95
|
6.07
|
1.12
|
27.8
|
3.85
|
Upp.V
|
>
and
|
242.35
|
259.38
|
17.03
|
4.57
|
0.62
|
15.2
|
3.53
|
Upp.V
|
NB20-009
|
40.30
|
84.00
|
43.70
|
4.76
|
0.43
|
18.9
|
3.64
|
Upp.
|
>
including
|
40.30
|
42.49
|
2.19
|
26.35
|
5.21
|
53.4
|
3.85
|
Upp.T/J
|
>>
including
|
41.40
|
42.49
|
1.09
|
44.80
|
8.33
|
77.6
|
3.81
|
Upp.T/J
|
NB20-009
|
181.00
|
406.00
|
225.00
|
2.08
|
0.09
|
5.3
|
2.97
|
Low.
|
>
including
|
181.00
|
212.00
|
31.00
|
2.99
|
0.03
|
5.2
|
2.93
|
Low.HP
|
>>
including
|
183.00
|
202.00
|
19.00
|
3.69
|
0.04
|
5.9
|
3.26
|
Low.HP
|
>>>
including
|
183.00
|
188.00
|
5.00
|
9.69
|
0.06
|
10.4
|
2.98
|
Low.HP
|
>
and
|
283.50
|
406.00
|
122.50
|
2.59
|
0.13
|
6.4
|
3.02
|
Low.V
|
>>
including
|
283.50
|
385.00
|
101.50
|
2.84
|
0.15
|
7.1
|
3.06
|
Low.V
|
>>>
including
|
315.00
|
365.00
|
50.00
|
3.75
|
0.12
|
5.6
|
3.08
|
Low.V
|
Upp.
= Upper Sequence;
Low. = Lower Sequence;
V = Vein mineralization;
T/J = Tom/Jason
style stratiform laminated mineralization;
HP = Howard's Pass style stratiform zinc
mineralization.
Averages are length and bulk density weighted.
CEO Statement
Brandon Macdonald,
CEO, stated "These
first
few
holes
into
the
new Boundary
West discovery
have
shown
the near-surface
upper
sequence to have
significant widths and grade, not just in the
newly discovered massive sulphide zone, but also within
the
barite-hosted stratiform mineralization which in NB20-009 has
shown grade
potential rivalling
the
best of Tom &
Jason.
The
lower
sequence at Boundary West shows similar
grades to parts of
central Boundary Zone
over a
225
m
intersection and the discovery
of mineralization in these older rocks hugely
expands the
exploration
space
for new discoveries across the
whole 940
km2
property.
These
initial
intersections
point
to two distinct stratiform mineralized
systems at
Boundary West that are each underlain by significant thicknesses of
vein mineralization.
Boundary
West remains open along
strike and down dip,
and
may
have continuity to central Boundary Zone to the east. This suggests
a massive size potential and a staggering metal
endowment."
NB20-009
and NB20-007
Drill Results
These
assays complete the
results for Fireweed's
new
2020
discovery, Boundary Zone West, approximately 360 m west of the
central area
of the
known Boundary Zone mineralized system. Drill hole
NB20-009
was
drilled on-section southwest of NB20-004 (Map
2), both
targeting
a
ground-gravity high anomaly surveyed earlier in the season.
Both
drill holes intersected
an
upper sequence comprising massive sulphides,
Boundary
Zone-style vein-hosted and replacement-style
mineralization, and
stratiform,
laminar zinc-lead-silver
mineralization
similar to
that
seen at Tom and Jason. NB20-009 also
intersected a lower sequence of stratiform, laminar
zinc
mineralization in
older host rocks which were
previously
not
believed to host
mineralization in the Macmillan Pass district (Section
1).
This
lower sequence is hosted in Late Ordovician-Early Silurian host
rocks the same age as host rocks at Howard's Pass,
90
km to
the southeast. Its discovery has significant implications for
exploration and dramatically
increases the area of prospective
host rocks in the
district.
Hole
NB20-007 encountered drilling problems at 90 m
depth and was
re-drilled from the same pad,
as NB20-009, intersecting
similar geology in the first 90 m.
NB20-008 Drill Results
Hole NB20-008 was
drilled as a step-out hole
85
m west
of pre-2020 drilling, between the previously known core of
mineralization at Boundary Zone and Boundary Zone West. Like
NB20-004 and NB20-009, NB20-008 targeted a ground gravity
high
anomaly. Sulphide mineralization included breccia and vein-hosted,
and replacement-style mineralization similar to
mineralization
seen in the core of the Boundary Zone system.
The true thickness
of the stratiform mineralization cannot be accurately
estimated yet
owing
to the variable orientation of nearby oriented core bedding
measurements and
sparsity
of
drill holes. The true
thickness of the stratiform mineralization in holes NB20-009 and
NB20-007 is estimated to be between 20% to 80% of intersected
thicknesses. True widths of individual cm- to m-scale veins
intersected in NB20-007, NB20-008 and NB20-009 vary greatly from
20% to 95% of intersected thicknesses reflecting the stockwork
nature of the veins, and at this early stage of drilling the
overall true thickness of Boundary Zone West cannot be accurately
estimated until further
drilling is completed.
Boundary Zone Potential
There is no
Mineral
Resource
for Boundary Zone yet
and
the zone is not included in the current mineral resource estimate
for the property (described in Fireweed news release dated January
10, 2018). Boundary Zone has potential to be mined in an open pit
with a low strip ratio and to be upgraded through low cost,
pre-concentration
ore sorting processes
(see
Fireweed news release dated July 31, 2019).
Recent drill results at Boundary Zone along with Tom North Zone and
End Zone (see Fireweed news releases dated August
20th
and
September 10th,
2019;
November 15th
and
29th,
2018;
January
26th,
2021) represent
potential for expansion of the large current mineral
resources on the
property and improvement of
Macmillan Pass project economics
described in the current Preliminary Economic Assessment (PEA) (see
Fireweed news release dated May 23rd,
2018).
Boundary Zone Background
Boundary Zone
mineralization consists of sphalerite-siderite-pyrite and minor
galena in veins, stockworks, disseminations, and as
replacement of
matrix and clasts within coarse clastic rocks. Drilling in 2020
at Boundary Zone West also identified stratiform
mineralization
similar to
the
Tom and Jason deposits (see news release
dated November 24th,
2020).
Historical
exploration work at Boundary Zone included geochemical and
geophysical surveys as well as 24 drill holes that defined a
central 200 x 800 m mineralized zone of zinc (-lead-silver)
mineralization within a broader system over 2 km in strike
length. Historical
length-weighted
average intersections1
such
as 224.0 m of 2.50% zinc and 0.30% lead, including 4.5 m of 16.40%
zinc, are consistent
with recent Fireweed drilling and demonstrated
potential for bulk tonnage open pit mineralization.
In 2019, Fireweed
drilled two holes into the central part of the known Boundary Zone
mineralization. Both holes intersected wide zones of high-grade
replacement-style and vein- and breccia-hosted zinc mineralization,
including 100.0 m (true
width) of 8.73% zinc from surface including 6.4 m of 43.53% zinc
within 230.0 m of 4.51% zinc (see Fireweed news
releases
dated
November 5th,
2019 and
January
26th,
2021).
In
2020 Fireweed drilled the discovery holes into the Boundary West
Zone described in this news release.
Notes on sampling,
assaying,
and data aggregation:
The
diamond
drill
core logging and sampling program was
carried out under
a rigorous quality assurance / quality control program using
industry best practices. Drill intersections in this
release are all
HQ3
(split tube) size core (61.1mm / 2.4-inch diameter) with recoveries
typically above 85%. After drilling, core was
logged
for geology, structure
and
geotechnical characteristics, marked for sampling, and photographed
on site. The cores for analyses were
marked
for sampling based on geological intervals with individual samples
1.5 m
or
less in length. Drill core from
the Boundary Zone was cut lengthwise in half with a core saw;
half-core was sent for assays reported in this news release, and
the other half is stored on site for reference. Bulk density was
determined on site for the entire length of each sample assayed by
measurement of mass in air and mass in water. Sample duplicate bulk
density determinations and in-house bulk density standard
determinations were each made at a rate of 5%. Since 2017, four
in-house bulk density standards (mineralized drill core from the
Tom deposit that span a range of densities) have been used and show
an acceptable long-term precision. Certified standard masses are
used to calibrate the scale balance used for bulk density
determinations.
A total of 5%
assay standards or blanks
and
5% core
duplicates are
included in
the
sample stream as a quality
control measure and are
reviewed after
analyses are
received. Standards and
blanks in 2020 drill results to date have been approved as
acceptable.
Duplicate data add
to the long-term estimates of precision for assay data on the
project and precision for drill results reported is deemed to be
within acceptable levels. Samples
were
sent
to the Bureau Veritas preparation laboratory in Whitehorse,
Yukon,
where
the samples were
crushed and
a 500
g split was sent to the Bureau
Veritas laboratory in Vancouver, B.C to be
pulverized to 85%
passing 200 mesh size pulps. Clean crush
material was passed through the crusher and clean silica was
pulverized between each sample. The pulps were analyzed by 1:1:1
Aqua Regia digestion followed by Inductively Coupled Plasma Mass
Spectrometry (ICP-ES/ICP-MS) multi-element analyses (BV Code
AQ270). All samples were
also
analyzed for multiple
elements by lithium borate
fusion and X-ray
fluorescence analysis (XRF) finish (BV Code LF725). Over-limit Pb
(>25.0%) and Zn (>24.0%)
were analyzed by lithium borate fusion with XRF finish (BV Code
LF726). Silver is reported
in this news release by method AQ270, and zinc and lead are
reported by LF725 or LF726. Bureau Veritas
(Vancouver) is an independent, international ISO/IEC 17025:2005
accredited laboratory.
Results in this
news release are length and bulk-density weighted averages as would
be used in a Mineral Resource estimate. Readers are cautioned that
in Fireweed news releases in prior years, only length weighted
assay averages were reported which may result in slightly lower
(under reported) average values. Length and bulk-density weighted
averages have been reported as these most accurately represent the
average metal-content of the intersections.
Qualified Person Statement
Technical
information in this news release has been approved by Gilles
Dessureau, P.Geo,
Vice President Exploration and a 'Qualified Person' as defined
under Canadian National Instrument 43-101.
About Fireweed Zinc Ltd. (TSXV: FWZ): Fireweed Zinc is a
public mineral exploration company focused on
zinc-lead-silver
and
managed by a veteran team of mining industry professionals. The
Company is advancing its district-scale 940
km2
Macmillan
Pass
Project in Yukon, Canada, which is host to the 100% owned Tom and
Jason zinc-lead-silver deposits with current Mineral Resources and
a PEA economic study (see Fireweed news releases dated January 10,
2018, and May 23, 2018, respectively, and reports filed on
www.sedar.com for details) as
well as the Boundary Zone, Tom North Zone and End Zone which have
significant zinc-lead-silver mineralization drilled but not yet
classified as mineral resources. The project also includes large
blocks of adjacent claims (MAC, MC, MP, Jerry, BR, NS, Oro, Sol,
Ben, and Stump) which cover exploration targets in the district
where previous and recent work identified zinc, lead and silver
prospects, and geophysical and geochemical anomalies in prospective
host geology.
Additional
information about Fireweed Zinc and its Macmillan Pass
Zinc
Project
including maps and
drill sections can be found on
the Company's website at
www.FireweedZinc.com and at
www.sedar.com.
ON BEHALF OF FIREWEED ZINC LTD.
"Brandon
Macdonald"
CEO &
Director
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.
Cautionary
Statements
This news release
may contain "forward-looking" statements and information relating
to the Company and the Macmillan Pass Project that are based on the
beliefs of Company management, as well as assumptions made by and
information currently available to Company management. Such
statements reflect the current risks, uncertainties and assumptions
related to certain factors including but not limited to, without
limitations, exploration and development risks, expenditure and
financing requirements, general economic conditions, changes in
financial markets, the ability to properly and efficiently staff
the Company's operations, the sufficiency of working capital and
funding for continued operations, title matters, First Nations
relations, operating hazards, political and economic factors,
competitive factors, metal prices, relationships with vendors and
strategic partners, governmental regulations and oversight,
permitting, seasonality and weather, technological change, industry
practices, and one-time events. Additional risks are set out in the
Company's prospectus dated May 9,
2017,
and
filed
under the Company's profile on SEDAR at
www.sedar.com.
Should
any one or more risks or uncertainties materialize or change, or
should any underlying assumptions prove incorrect, actual results
and forward-looking statements may vary materially from
those described herein.
The Company does not undertake to update forward-looking statements
or forward-looking
information,
except as required by law.
Footnotes:
1.
Historic results for the Boundary Zone reported in this news
release are taken from historic reports prepared by previous
operators. Neither the Company or the Qualified Person has done
sufficient work to verify these results and therefore these results
should not be relied upon. The Company is including them for
information purposes to explain the basis for the exploration
target and reasons for drilling.
Map 1 –
Macmillan Pass
Project:
Locations of the
2020 exploration targets, advanced prospects, and known
deposits.
Map
2
–
Boundary
Zone:
Locations of
the 2020 diamond drill
holes and cross-section B-B'.
Section
1:
Boundary
Zone
West Cross-Section
B-B'.
Table
2:
Full
results from NB20-007.
Hole
|
From (m)
|
To (m)
|
Intersection (m)
|
Zinc (%)
|
Lead (%)
|
Silver (g/t)
|
Bulk Density (t/m3)
|
Zone
|
NB20-007
|
37.00
|
72.00
|
35.00
|
3.90
|
0.30
|
14.6
|
3.20
|
Upp.
|
>
including
|
37.00
|
53.00
|
16.00
|
6.96
|
0.54
|
20.7
|
3.30
|
Upp.
|
>>
including
|
37.00
|
46.55
|
9.55
|
9.74
|
0.81
|
27.0
|
3.47
|
Upp.
|
>>>
including
|
37.00
|
38.68
|
1.68
|
26.13
|
3.36
|
36.8
|
3.39
|
Upp.T/J
|
>>>
and
|
43.60
|
46.55
|
2.95
|
12.94
|
0.41
|
47.3
|
4.26
|
Upp.V
|
>>
and
|
51.00
|
53.00
|
2.00
|
6.14
|
0.09
|
14.4
|
3.07
|
Upp.V
|
Upp.
= Upper Sequence.
V = Vein mineralization.
T/J = Tom/Jason style stratiform laminated mineralization.
Averages are length and bulk density weighted.
Table
3:
Full
results from NB20-008.
Hole
|
From (m)
|
To (m)
|
Intersection (m)
|
Zinc (%)
|
Lead (%)
|
Silver (g/t)
|
Bulk Density (t/m3)
|
Zone
|
NB20-008
|
27.00
|
27.89
|
0.89
|
5.76
|
0.02
|
6.9
|
3.37
|
Vein
|
NB20-008
|
70.00
|
72.00
|
2.00
|
2.68
|
0.41
|
6.2
|
2.61
|
Vein
|
NB20-008
|
90.00
|
114.00
|
24.00
|
2.10
|
0.18
|
5.9
|
2.75
|
Vein
|
>
including
|
100.00
|
114.00
|
14.00
|
3.08
|
0.30
|
8.8
|
2.78
|
Vein
|
>>
including
|
108.00
|
110.09
|
2.09
|
11.33
|
0.02
|
15.3
|
2.93
|
Vein
|
NB20-008
|
148.00
|
149.50
|
1.50
|
3.76
|
0.09
|
4.1
|
2.81
|
Vein
|
NB20-008
|
194.83
|
306.00
|
111.17
|
2.48
|
0.74
|
12.5
|
3.37
|
Upp.V
|
>
including
|
198.05
|
212.00
|
13.95
|
6.07
|
1.12
|
27.8
|
3.85
|
Upp.V
|
>>
including
|
204.00
|
212.00
|
8.00
|
7.95
|
1.10
|
29.5
|
3.6575
|
Upp.V
|
>
and
|
235.00
|
240.00
|
5.00
|
1.46
|
0.81
|
8.4
|
3.41
|
Upp.V
|
>
and
|
242.35
|
259.38
|
17.03
|
4.57
|
0.62
|
15.2
|
3.53
|
Upp.V
|
>
and
|
289.00
|
290.00
|
1.00
|
9.77
|
0.76
|
19.7
|
3.38
|
Upp.V
|
Upp.
= Upper Sequence.
V = Vein mineralization.
Averages are length and bulk density weighted.
Table
4:
Full
results from NB20-009.
Hole
|
From (m)
|
To (m)
|
Intersection (m)
|
Zinc (%)
|
Lead (%)
|
Silver (g/t)
|
Bulk Density (t/m3)
|
Zone
|
NB20-009
|
40.30
|
84.00
|
43.70
|
4.76
|
0.43
|
18.9
|
3.64
|
Upp.
|
>
including
|
40.30
|
69.85
|
29.55
|
5.66
|
0.58
|
21.6
|
3.71
|
Upp.
|
>>
including
|
40.30
|
42.49
|
2.19
|
26.35
|
5.21
|
53.4
|
3.85
|
Upp.T/J
|
>>>
including
|
41.40
|
42.49
|
1.09
|
44.80
|
8.33
|
77.6
|
3.81
|
Upp.T/J
|
>>
and
|
46.26
|
51.00
|
4.74
|
7.87
|
0.35
|
33.3
|
4.33
|
Upp.V
|
NB20-009
|
164.00
|
167.00
|
3.00
|
2.85
|
0.04
|
7.2
|
3.22
|
Vein
|
NB20-009
|
181.00
|
406.00
|
225.00
|
2.08
|
0.09
|
5.3
|
2.97
|
Low.
|
>
including
|
181.00
|
212.00
|
31.00
|
2.99
|
0.03
|
5.2
|
2.93
|
Low.HP
|
>>
including
|
183.00
|
202.00
|
19.00
|
3.69
|
0.04
|
5.9
|
3.26
|
Low.HP
|
>>>
including
|
183.00
|
188.00
|
5.00
|
9.69
|
0.06
|
10.4
|
2.98
|
Low.HP
|
>>>>
including
|
183.00
|
185.00
|
2.00
|
14.47
|
0.06
|
12.6
|
3.06
|
Low.HP
|
>>>>
and
|
186.00
|
188.00
|
2.00
|
8.98
|
0.07
|
11.8
|
3.00
|
Low.HP
|
>>>
and
|
195.00
|
197.00
|
2.00
|
5.87
|
0.02
|
6.8
|
2.79
|
Low.HP
|
>
and
|
283.50
|
406.00
|
122.50
|
2.59
|
0.13
|
6.4
|
3.02
|
Low.V
|
>>including
|
283.50
|
385.00
|
101.50
|
2.84
|
0.15
|
7.1
|
3.06
|
Low.V
|
>>>
including
|
296.32
|
298.71
|
2.39
|
7.23
|
0.16
|
19.1
|
3.93
|
Low.V
|
>>
and
|
315.00
|
365.00
|
50.00
|
3.75
|
0.12
|
5.6
|
3.08
|
Low.V
|
>>>
including
|
315.00
|
316.00
|
1.00
|
14.50
|
0.22
|
15.3
|
3.60
|
Low.V
|
>>>
and
|
329.70
|
334.05
|
4.35
|
6.54
|
0.24
|
9.2
|
3.26
|
Low.V
|
>>>
and
|
341.00
|
342.00
|
1.00
|
15.08
|
0.38
|
12.3
|
3.67
|
Low.V
|
>>>
and
|
350.00
|
351.00
|
1.00
|
17.29
|
0.04
|
6.3
|
3.26
|
Low.V
|
>>>
and
|
355.00
|
356.00
|
1.00
|
11.73
|
0.02
|
5.1
|
3.27
|
Low.V
|
>>>
and
|
360.00
|
365.00
|
5.00
|
5.42
|
0.04
|
9.0
|
2.96
|
Low.V
|
>>
and
|
397.13
|
406.00
|
8.87
|
2.48
|
0.02
|
2.5
|
2.94
|
Low.V
|
Upp.
= Upper Sequence; Low. = Lower Sequence.
V = Vein mineralization.
T/J = Tom/Jason style stratiform laminated mineralization.
HP = Howard's Pass style stratiform zinc mineralization.
Averages are length and bulk density weighted.
Table
5: 2020 drill hole
collar data.
Diamond Drill Hole
Collars
Drill Hole
|
Length (m)
|
Zone
|
Easting*
|
Northing*
|
Elevation (m)
|
Dip (°)
|
Grid Azimuth (°)
|
NB20-001
|
303.5
|
Boundary
Zone
|
422440
|
7010418
|
1164
|
-54
|
270
|
NB20-002
|
320.0
|
Boundary
Zone
|
422336
|
7010329
|
1132
|
-50
|
020
|
NB20-003
|
152.0
|
Boundary
Zone
|
421557
|
7010456
|
1200
|
-50
|
185
|
NB20-004
|
333.0
|
Boundary
Zone
|
422049
|
7010614
|
1218
|
-50
|
215
|
NB20-005
|
143.0
|
Boundary
Zone
|
422277
|
7010313
|
1129
|
-50
|
215
|
NB20-006
|
203.0
|
Boundary
Zone
|
422277
|
7010313
|
1129
|
-80
|
215
|
NB20-007
|
90.0
|
Boundary
Zone
|
421951
|
7010538
|
1200
|
-70
|
215
|
NB20-008
|
324.0
|
Boundary
Zone
|
422216
|
7010354
|
1139
|
-50
|
215
|
NB20-009
|
447.2
|
Boundary
Zone
|
421951
|
7010538
|
1200
|
-75
|
215
|
MP20-001
|
632.0
|
240
Mile
|
438698
|
7003094
|
1311
|
-60
|
295
|
*UTM Zone 9 NAD83
Reverse
Circulation (RC) Drill Hole Collars
Drill Hole
|
Length (m)
|
Zone
|
Easting*
|
Northing*
|
Elevation (m)
|
Dip (°)
|
Grid Azimuth (°)
|
TRC20-001
|
7.6
|
Tom
West
|
442065
|
7003667
|
1547
|
-50
|
066
|
TRC20-002
|
82.3
|
Tom
West
|
442071
|
7003663
|
1547
|
-80
|
066
|
TRC20-003
|
64.0
|
Tom
West
|
442071
|
7003663
|
1547
|
-55
|
066
|
TRC20-004
|
64.0
|
Tom
West
|
442071
|
7003663
|
1547
|
-70
|
089
|
TRC20-005
|
47.2
|
Tom
West
|
442071
|
7003663
|
1547
|
-55
|
129
|
TRC20-006
|
36.6
|
Tom
West
|
442049
|
7003678
|
1545
|
-80
|
065
|
TRC20-007
|
98.45
|
Tom
North
|
441654
|
7004507
|
1422
|
-51
|
076
|
JRC20-001
|
47.24
|
Jason
Main
|
436437
|
7002774
|
1298
|
-50
|
027
|
JRC20-002
|
59.44
|
Jason
Main
|
436533
|
7002772
|
1300
|
-65
|
011
|
*UTM Zone 9 NAD83
Table
6:
2020
drill hole results and observations.
Diamond Drill Hole
Descriptions
Drill Hole
|
Length (m)
|
Zone
|
Target
|
Results and Observations
|
NB20-001
|
303.5
|
Boundary
Zone
|
BZ core
infill
|
Wide zone
encountered. Results reported
in prior
news
release.
|
NB20-002
|
320.0
|
Boundary
Zone
|
BZ core
infill/step-out
|
Wide zone
encountered. Hole abandoned at 320 m in mineralization due to
drilling problems. Results reported
in prior
news
release.
|
NB20-003
|
152.0
|
Boundary
Zone
|
Gravity high
anomaly ~800 m west of BZ
|
No significant
mineralization. Gravity
anomaly explained by dense
sedimentary rock unit
|
NB20-004
|
333.0
|
Boundary
Zone
|
Gravity high
anomaly 360 m west of BZ
|
Wide zone
encountered. Reported in
prior
news
release.
|
NB20-005
|
143.0
|
Boundary
Zone
|
BZ step-out to
south
|
No significant
mineralization.
|
NB20-006
|
203.0
|
Boundary
Zone
|
BZ step-out to
south
|
Minor
mineralization encountered.
|
NB20-007
|
90.0
|
Boundary
Zone
|
Gravity high 360 m
W of BZ
|
Hole abandoned due
to drilling problems and re-drilled as NB20-009.
Reported
in this news release.
|
NB20-008
|
324.0
|
Boundary
Zone
|
Gravity high
anomaly 200 m
west of BZ and step-out 80 m west of previous drilling
|
Wide zone
encountered. Reported in this
news release.
|
NB20-009
|
447.2
|
Boundary
Zone
|
Gravity high
anomaly 360 m W of BZ
|
Wide zone
encountered. Reported in this
news release.
|
MP20-001
|
632.0
|
240 Mile
Target
|
Gravity high
anomaly between the Tom and Jason deposits
|
Hole suspended
before reaching target horizon; casing left in place to allow
resumption of drilling next season.
|
Reverse
Circulation (RC) Drill Hole Descriptions – assays
pending.
Drill Hole
|
Length (m)
|
Zone
|
Target
|
Results and Observations
|
TRC20-001
|
7.6
|
Tom
West
|
Infill
|
Hole abandoned at
casing due to drilling problems
|
TRC20-002
|
82.3
|
Tom
West
|
Infill
|
Tom West zone
intersected. Assays
pending.
|
TRC20-003
|
64.0
|
Tom
West
|
Infill
|
Tom West zone
intersected.
Assays
pending.
|
TRC20-004
|
64.0
|
Tom
West
|
Twin of historic
hole
|
Successful twin
with good recovery. Assays
pending.
|
TRC20-005
|
47.2
|
Tom
West
|
Step-out
|
Hole abandoned
before target depth due to drilling problems
|
TRC20-006
|
36.6
|
Tom
West
|
Infill
|
Hole abandoned
before target depth due to drilling problems
|
TRC20-007
|
98.45
|
Tom
North
|
Infill
|
Tom North zone
intersected. Assays
pending.
|
JRC20-001
|
47.24
|
Jason
Main
|
Infill
|
Jason Main zone
intersected. Assays
pending.
|
JRC20-002
|
59.44
|
Jason
Main
|
Infill
|
Jason Main zone
intersected. Hole abandoned in
mineralization. Assays pending.
|
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