Hemlo Explorers Inc. (the “Company”) (TSXV: HMLO) announced today
the final drill results from it’s 18-hole 7,891 m program (Table 1)
at the North Limb project, located 15 km north of Barrick Gold
Corporation’s Hemlo Mine near Marathon, Ontario.
Highlights:
- Armand Lake Volcanic Complex
(“ALVC”) Lunny East Showing: Drillholes NL21-12 (Section L+900),
NL21-13 (Section L+350), NL21-14, -15 (Section L-1140), NL21-16
(Section L+1100), NL21-17 (Section L+800) and NL21-18 (Section
L+1350) totalling 2,396.15 m were drilled on five sections over a
strike length of 1,000 m (Figure 1). These holes were designed to
test the North and Southern contacts of the ALVC, areas of possible
folding and elevated gold, antimony and molybdenum in surface rock
and soil sampling.
- Drilling intercepted anomalous gold
horizons on all sections (Figures 2-7, Table 2) and can be
correlated to surface sampling in holes NL21-13, -16 and -17 over
vertical distances of approximately 275 metres, 175 metres and 150
metres, respectively.
- All available historical drillhole
data has been now successfully digitally captured and 3D© Leapfrog
drillhole and geochemical modelling is ongoing and additional
drillhole planning is being evaluated for future exploration.
As has been reported with previous drill results
from the Musher, Armand and Lunny West showings, multi-element ICP
data using ioGAS© geochemical software has identified widespread
pathfinder elements such as Ag, Sb, Mo, As, V, Te, +/- Hg Cu and Zn
at the Lunny East showing. Some of these elements have been
positively correlated with Au mineralization at the nearby Hemlo
Mine, while others define broader horizons indicating a more
extensive corridor of hydrothermal activity.
Brian Howlett, CEO of Hemlo Explorers, commented
“We are satisfied that our initial drill program at the North Limb
project demonstrated widespread anomalous gold horizons that can be
in some instances correlated over considerable vertical depth.
Additionally, extensive elevated pathfinder elements, as seen at
the Hemlo Mine, defined a broad hydrothermal system over a strike
length of in excess of 5 kilometres covering a large portion of the
ALVC trend.”
Figure #1: Armand Lake Volcanic Complex
Drillhole Plan Map, Lunny
Areahttps://www.globenewswire.com/NewsRoom/AttachmentNg/e6c4aa7b-aec7-4657-ba02-331aa46fb7df
Figure #2: Section L+900
(NL21-12)https://www.globenewswire.com/NewsRoom/AttachmentNg/583faee0-11b5-4a10-913a-8a69a9683814
Figure #3: Section L+350
(NL21-13)https://www.globenewswire.com/NewsRoom/AttachmentNg/105746ce-1403-4866-9aa2-23f4b5361866
Figure #4: Section L+1140 (NL21-14,
-15)https://www.globenewswire.com/NewsRoom/AttachmentNg/09ba5850-a5b9-4549-ba8c-a6ac10fed067
Figure #5: Section L+1100
(NL21-16)https://www.globenewswire.com/NewsRoom/AttachmentNg/7b4026c7-6069-4fbf-8f6a-18c631c60215
Figure #6: Section L+800
(NL21-17)https://www.globenewswire.com/NewsRoom/AttachmentNg/5aaaaeda-05fc-4a73-9d75-1cb8005436ac
Figure #7: Section L+800
(NL21-18)https://www.globenewswire.com/NewsRoom/AttachmentNg/61b83b41-9b6f-4530-9dca-ae2021ef4d23
Table 1. Drill Collar Coordinates |
Hole ID |
Easting |
Northing |
Elevation |
Azimuth |
Dip |
Length |
NL21-01 |
589174 |
5409003 |
372 |
20 |
-45 |
332.00 |
NL21-02 |
589267 |
5408836 |
351 |
20 |
-65 |
626.17 |
NL21-03 |
589081 |
5408822 |
352 |
20 |
-65 |
629.00 |
NL21-04 |
589081 |
5408822 |
352 |
20 |
-56 |
439.90 |
NL21-05 |
589084 |
5409229 |
356 |
200 |
-60 |
440.00 |
NL21-06 |
590228 |
5409135 |
370 |
20 |
-65 |
510.00 |
NL21-07 |
591079 |
5408821 |
357 |
20 |
-55 |
531.00 |
NL21-08 |
590984 |
5408667 |
374 |
20 |
-55 |
420.00 |
NL21-09 |
590804 |
5408998 |
357 |
20 |
-50 |
436.50 |
NL21-10 |
586137 |
5409853 |
367 |
0 |
-60 |
575.07 |
NL21-11 |
586356 |
5410031 |
385 |
180 |
-55 |
549.00 |
NL21-12 |
587651 |
5410000 |
396 |
0 |
-45 |
312.00 |
NL21-13 |
587091 |
5409974 |
385 |
180 |
-50 |
427.50 |
NL21-14 |
587894 |
5409793 |
374 |
0 |
-45 |
396.00 |
NL21-15 |
587894 |
5409793 |
374 |
0 |
-63 |
207.00 |
NL21-16 |
587868 |
5409698 |
373 |
180 |
-50 |
408.00 |
NL21-17 |
587523 |
5409963 |
399 |
0 |
-51 |
400.00 |
NL21-18 |
588103 |
5409783 |
372 |
0 |
-60 |
252.00 |
Table 2. Summary of Current and Historic Drill Results for
the Lunny Area |
Section |
Hole ID |
From (m) |
To (m) |
Intersection Width (m) |
Au (ppb) |
Comments |
L+900 |
NL21-12 |
115.70 |
117.95 |
2.25 |
25 |
V, Sb, Ag +/-Mo, As, Te, Hg |
|
NL21-12 |
123.50 |
126.10 |
2.60 |
67 |
|
|
NL21-12 |
137.05 |
137.65 |
0.60 |
461 |
|
L+350 |
NL21-13 |
199.49 |
200.58 |
1.09 |
36 |
Ag, V +/- Mo, As, Te, Hg, Cu, Zn |
|
NL21-13 |
331.31 |
332.80 |
1.49 |
55 |
|
|
NL21-13 |
350.37 |
351.75 |
1.38 |
156 |
|
|
NL21-13 |
381.96 |
383.33 |
1.37 |
83 |
|
|
NL21-13 |
388.62 |
389.43 |
0.81 |
1,400 |
1.40 g Au/t |
L+1140 |
NL21-14 |
85.15 |
85.50 |
0.35 |
215 |
Ag, Mo, Sb, Cu +/- V, Te, As |
|
NL21-14 |
382.50 |
384.00 |
1.50 |
163 |
|
L+1140 |
NL21-15 |
48.00 |
48.30 |
0.30 |
252 |
Ag, Mo, Cu +/- Sb |
|
NL21-15 |
57.58 |
58.21 |
0.63 |
76 |
|
|
NL21-15 |
87.52 |
88.50 |
0.98 |
38 |
|
|
NL21-15 |
191.52 |
192.22 |
0.70 |
23 |
|
L+1100 |
NL21-16 |
36.70 |
38.50 |
1.80 |
24 |
Ag, Mo, Cu +/- Sb, V, Te |
|
NL21-16 |
50.50 |
53.50 |
3.00 |
24 |
|
|
NL21-16 |
65.25 |
4.85 |
4.85 |
48 |
|
|
NL21-16 |
151.15 |
153.60 |
2.45 |
30 |
|
|
NL21-16 |
241.20 |
242.40 |
1.20 |
36 |
|
L+800 |
NL21-17 |
18.40 |
20.55 |
2.15 |
50 |
Ag, Mo, Cu, Sb, As +/- V, Te, Hg, Zn |
|
NL21-17 |
24.50 |
26.29 |
1.79 |
21 |
|
|
NL21-17 |
122.50 |
124.41 |
1.91 |
24 |
|
|
NL21-17 |
204.10 |
207.00 |
2.90 |
151 |
|
|
NL21-17 |
235.15 |
239.50 |
4.35 |
69 |
|
|
NL21-17 |
285.16 |
287.15 |
1.99 |
27 |
|
|
N-96-02 (Historic) |
40.22 |
42.00 |
1.78 |
68 |
|
L+1350 |
NL21-18 |
240.16 |
240.64 |
0.48 |
43 |
Ag, Mo, Cu +/-Sb, V, Te |
The North Limb geological setting resembles that
of the Hemlo Mine with felsic to intermediate volcanic and
sedimentary assemblages, quartz-feldspar intrusives in a district
scale, high strain arcuate structural regime. Much of the
mineralization at the Hemlo Mine is confined to high strain zones
and spatially associated with the contact between felsic volcanic
rocks and sedimentary rocks. Similar alteration of silica,
sericite, feldspar and vanadium to that of the Hemlo Deposit is
found with anomalous gold along the Armand and Musher Horizons
which have strike lengths of 7 and 8 kilometres, respectively.
Quality Assurance – Quality
Control
Once received from the drill and processed, all
drill core samples are sawn in half, labelled and bagged. The
remaining drill core is securely stored on site. Numbered security
tags are applied to lab shipments for chain of custody
requirements. The Company inserts quality control (QC) samples at
regular intervals in the sample stream, including blanks and
reference materials with all sample shipments to monitor and
evaluate laboratory performance. The QA/QC program was designed by
Dan McCormack, PGO and is overseen by Dr. Lesley Rose, PGO.
Drill core samples are submitted to Activation
Laboratories’ analytical facility in Thunder Bay, Ontario for
preparation and analysis is completed at the Thunder Bay and
Ancaster facilities. Both labs are accredited to the ISO/IEC 17025
standard for gold and multi-element assays and all analytical
methods include quality control materials at set frequencies with
established data acceptance criteria. The entire sample is crushed
and 500 g is pulverized. Analysis for gold is by 30 g fire assay
fusion with atomic absorption (AAS) finish with a lower limit of
0.005 ppm (5 ppb) and upper limit of 5 ppm (5000 ppb). Samples with
gold assays greater than 2 ppm are re-analyzed using a 50 g fire
assay fusion with gravimetric finish. A selected number of samples
are also analyzed using a 60 element geochemical package by aqua
regia digestion, followed by a combination of Inductively Coupled
Plasma Optical Emission Spectroscopy (ICP-OES) and Inductively
Coupled Plasma Mass Spectrometry (ICP-MS) for analysis.
Technical Information
Mr. Adrian Bray, P.Geo., Exploration Manager for
the Company, is the “Qualified Person” as defined by National
Instrument 43-101 Standards of Disclosure for Mineral
Projects, responsible for the accuracy of technical information
contained in this news release.
About Hemlo Explorers Inc.
Hemlo Explorers is a Canadian-based mineral
exploration company with a portfolio of properties in Ontario and
Nunavut. We are focused on generating shareholder value through the
advancement of our main Hemlo area projects, including the North
Limb, Pic and Hemlo West.
For more information please contact:
Brian Howlett, President & CEOHemlo
Explorers Inc.brian@hemloexplorers.ca (647) 227-3035
http://www.hemloexplorers.ca
Forward-Looking Statements
Certain information set forth in this news
release may contain forward-looking statements that involve
substantial known and unknown risks and uncertainties, including,
but not limited to, exploration results, potential mineralization,
statements relating to mineral resources, and the Company’s plans
with respect to the exploration and development of its properties.
These forward-looking statements are subject to numerous risks and
uncertainties, certain of which are beyond the control of Hemlo
Explorers Inc., including, but not limited to, the impact of
general economic conditions, industry conditions, volatility of
commodity prices, risks associated with the uncertainty of
exploration results and estimates, currency fluctuations,
dependency upon regulatory approvals, the uncertainty of obtaining
additional financing, exploration risk and Covid-19 pandemic
related orders. Readers are cautioned that the assumptions used in
the preparation of such information, although considered reasonable
at the time of preparation, may prove to be imprecise and, as such,
undue reliance should not be placed on forward-looking
statements.
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