Harfang Exploration Inc. (“Harfang” or the “Company”) (TSX-V:
HAR
) is pleased to report analytical results from
drill holes recently completed on its Lake Menarik Gold Property
(“Property”) in Eeyou Istchee James Bay, Québec
(
Figure 1). The results reported today
confirm broad gold intervals in a highly altered and brecciated
monzonite that are open at depth in the Pierre and Pierre Ouest
areas, and gold mineralized zones at depth and along strike of the
David surface occurrence. The winter program also included an
Induced Polarization (“IP”) geophysical survey that highlighted
several chargeability targets in other areas of the Property that
will be followed up during the upcoming field program to begin in
June. The Property, located 45 kilometres south of Radisson
(Québec) consists of 304 claims (15,627 hectares) and is
100% owned by Harfang.
Drill Highlights:
- Pierre and Pierre Ouest Areas:
- 1.15 g/t Au over 47.0
metres including 3.75 g/t Au over 7.0
metres, and 1.05 g/t Au over 12.0 metres
(LMN-23-017);
- 1.75 g/t Au over 21.0
metres including 2.49 g/t Au over 14.1
metres (LMN-23-001);
- 0.54 g/t Au over 75.0
metres including 6.75 g/t Au over 3.0
metres and 12.65 g/t Au over 1.0
metre (LMN-23-004).
- David Area:
- 0.88 g/t Au over 9.45
metres including 5.19 g/t Au over 1.15
metres (LMN-23-009);
- 1.64 g/t Au over 5.3
metres including 6.68 g/t Au over 1.2
metres (LMN-23-011).
Commented Ian Campbell, President and CEO, “Our
maiden drill program of shallow drilling on the Property has
successfully demonstrated that wide zones of gold mineralization
associated with increasing intensity of alteration extend to depth
in the southeast area of the monzonite. We are excited about the
upcoming field campaign set to begin in early June which is
designed to generate additional drill targets, building on our
field campaign from last year where we made several discoveries to
the East of the drilled sector, and in areas which have had no work
completed to date.”
Geological Setting
The Property is characterized by multiple
high-grade gold occurrences hosted in a polyphase intermediate
intrusion (syenite, monzonite and monzodiorite) and adjacent
volcano-sedimentary rocks. The geological setting of the Property
is reminiscent of that of the Timmins Camp based on the occurrence
of gold-bearing monzonite/syenite intrusions, volcanic and
sedimentary rocks including a Timiskaming-type conglomerate, and
lamprophyres.
Discussion of the Results
This maiden phase of drilling by Harfang at Lake
Menarik consists of 17 shallow drill holes totalling
3,416 metres (Figures 2 and 3). Drilling
was primarily designed at testing the gold-enriched intrusive
monzonitic suite (the “Pierre monzonite”) for lateral and vertical
extensions of gold intervals obtained in very limited historic
shallow drilling completed in 2000. Other holes tested different
areas within the Pierre monzonite as well as its volcanic and
sedimentary host rocks and associated with chargeability targets
delineated by a previous IP survey, coincident with magnetic
variations and structural features. Table 1 lists
all gold intervals with a metal factor (g/t Au x metres) above 5 in
holes LMN-23-001 to LMN-23-017.
Table 1. Gold intervals with a metal factor
above 5 in holes LMN-23-001 to LMN-23-017*.*Assay intervals
reported are core lengths; true widths have not been
determined.
Five holes (LMN-23-001 to 004 and LMN-23-017)
targeted the Pierre and Pierre Ouest showings located within a
270-metre long by 90-metre wide monzonite outlier south of the main
Pierre monzonite (2,200 m x 300 m). These holes confirm
that gold intervals extend laterally and at depth within the
monzonite outlier which contains an anomalous gold background.
LMN-23-017 intersected two significant gold intervals in highly
sericitized and silicified monzonite that graded
1.15 g/t Au over 47.0 metres
(95.0-142.0 m), including 3.75 g/t Au over
7.0 metres (131.0-138.0 m), and
1.05 g/t Au over 12.0 metres
(158.0-170.0 m) (Figure 4). LMN-23-017, the
deepest hole drilled to date in this area, extends previously
drilled gold zones to a vertical depth of 140 metres.
LMN-23-001 tested the lateral continuity of the mineralization on
the northern edge of the intrusion outlier and returned
1.75 g/t Au over 21.0 metres
(62.0-83.0 m), including 2.49 g/t Au over
14.1 metres (64.0-78.1 m) (Figure
4).
Drill intercepts dominated by
chlorite-quartz-pyrite veining injected into the monzonite returned
anomalous gold zones assaying 0.54 g/t Au over
75.0 metres (6.0-81.0 m), including up to
6.75 g/t Au over 3.0 metres
(54.0-57.0 m) [LMN-23-004], 0.50 g/t Au over
17.0 metres (104.0-121.0 m) [LMN-23-002] and
0.30 g/t Au over 27.0 metres
[90.0-117.0 m) [LMN-23-003] (Figure 5).
Drilling has demonstrated that the sericite-rich gold zones are
more common at depth and along the northern and southern flanks of
the monzonite outlier. These zones extend in a westerly direction
and plunge steeply to the west.
All holes under Pierre and Pierre Ouest are
characterized by brecciated and highly altered monzonite with zones
of silicification, hematization, sericitization and albitization
with chlorite and quartz-carbonate veining. Pyrite, the most common
sulphide, occurs disseminated in the altered matrix of the
monzonite, in chlorite veinlets and in quartz-carbonate veins and
stockworks. The best gold intervals are associated with
sericitization, silicification (veins and silica flooding) and
pyrite (Figure 4).
Holes LMN-23-006 to 014 tested a variety of gold
showings coincident with mapped and/or interpreted structural
lineaments, and IP chargeability targets in the main Pierre
monzonite (Figure 2). LMN-23-006 to 008
targeted the contact of the intrusion with the volcano-sedimentary
host rocks underneath Benoit (2.53 g/t Au over 4.72 m
[1404-05]) and Giaro (up to 2.37 g/t Au over 2.36 m
[1404-14]). Visible gold was observed in a monzonite-hosted quartz
vein in LMN-23-008 which returned 6.20 g/t Au over
0.3 metres within an anomalous interval of
0.57 g/t Au over 13.2 metres
(219,3-232,5 m).
Three holes (LMN-23-009 to 011) tested
structural lineaments and IP targets in the vicinity of the David
showing. Significant gold intervals dominated by monzonite-hosted
quartz veins, locally associated with shear zones, were
intersected: 0.88 g/t Au over
9.45 metres (207.05-216.50 m) including
5.19 g/t Au over 1.15 metres, and 5.04 g/t
Au over 1,0 metre (223,1-224,1 m) in LMN-23-009,
1.16 g/t Au over 4.7 metres (6.0-17.0 m) in
LMN-23-010, and 1.64 g/t Au over 5.3 metres
(99.1-104.4 m) including 6.68 g/t Au over
1.2 metres in LMN-23-011.
Six holes (LMN-23-005, LMN-23-007, LMN-23-013 to
016) tested the northern contact of the Pierre monzonite and/or
prominent ENE-WSW sedimentary-hosted structural lineaments to the
north and east of the Pierre monzonite coincident with IP
chargeability targets (Figure 2). Drilled
lithologies include wacke, siltstone, conglomerate and mafic
volcanics containing wide pyrite-bearing shear zones with
boudinaged, folded and irregular quartz veins. No significant gold
intervals were intersected.
2023 Induced Polarization
Survey
An IP survey consisting of 39.2 linear
kilometres was completed in March. The survey covered the eastern
and northern portions of the Pierre monzonite and deformation
corridors between the volcano-sedimentary rocks and the
Timiskaming-type conglomerate (Figure 6).
Three lines were also surveyed over the ankerite-rich sheared
corridor at least 700 metres long and 50 metres wide in
the eastern part of the Property (see news release dated January
12, 2023). Among the many IP anomalies detected by the survey,
strong and wide chargeability targets at least 1.5 kilometres
long have been outlined near the contact between the
volcano-sedimentary package and the conglomerate. This geological
setting, which marks a first-priority structural interface with the
potential of hosting mineralization, and several other IP targets
will be prospected during the summer.
Field Work Set to Begin
Harfang is in the final preparation stage for
the summer field campaign set to begin in early June and designed
to advance several additional targets to the drilling stage. The
program will focus on advancing the overall understanding of the
geological model east of the Pierre monzonite and several
attractive target areas. These include the Timiskaming-type
conglomerate and its associated IP anomalies, the Greco gold
showing adjacent to mining claims acquired last fall (1.04 g/t
Au over 24.9 metres [channel]), and building on discoveries
from the 2022 program such as the Oswald showing (17.30 g/t
Au, 217 g/t Ag and 0.61% Pb [grab] and up to 6.34 g/t Au,
60 g/t Ag and 0.09% Pb over 0.40 m [channel]) and the
ankerite zones (up to 2.87 g/t Au in grab samples) (Figure
6). This program has been enhanced by recent geophysical
data from the IP survey and the detailed heliborne magnetic
survey.
Harfang is also preparing its summer program on
its new lithium properties, whose exploration targets have been
developed based on the combination of geological criteria and the
presence of lithium anomalies in lake bottom sediments.
QA/QC and Core Sampling
Protocols
Drill core was transported from the drill rig to
the logging facility in Radisson where it was logged, photographed,
and split by diamond saw under the supervision of Harfang
geologists. The samples collected at regular intervals were then
individually bagged, and blanks and certified reference materials
were inserted. Individual samples were placed in large bags and
sent to ALS (Val-d’Or, Québec) to be analyzed for gold and 33 other
chemical elements. Gold was analyzed by atomic absorption following
fire assaying on a 30-gram sample fraction (Au-AA23). Other
elements were analyzed using the four-acid ICP–AES method
(ME-ICP61). Samples with >10 g/t Au were reanalyzed with a
gravimetric finish (Au-GRA21). Sample preparation and analytical
determination were performed in various ALS laboratories.
The sampling procedures and the quality control
followed protocols developed by Harfang and ALS. Preliminary data
interpretation was done by Harfang.
Qualified Person
The technical information in this news release
was prepared and approved by François Huot, P.Geo, Vice President
Exploration of Harfang, who is a non-independent qualified person
for the technical disclosure as defined by the National Instrument
43-101 Standards of Disclosure for Mineral Projects
(“NI43-101”).
About Harfang Exploration
Inc.
Harfang Exploration Inc. is well financed with
approximately $7.4 M in the treasury as of March 31, 2023 and
is a technically driven mineral exploration company with the
primary mission to discover ore deposits in Québec and Ontario. The
Company is managed by an experienced team of industry professionals
with a proven track record of success, controls a portfolio of
highly prospective projects and has a strong financial position.
Harfang is dedicated to best practices through engagement with all
stakeholders and commitment to the environment.
On behalf of the Board of Directors and for further
information, please contact:
Ian CampbellPresident and Chief Executive OfficerTel:
647 680-3820Email: icampbell@harfangexploration.comWeb:
www.harfangexploration.com
Cautionary Statement Regarding Forward-Looking
Information
The information in this news release includes
certain information and statements about management’s view of
future events, expectations, plans and prospects that constitute
forward-looking statements. These statements are based upon
assumptions that are subject to significant risks and
uncertainties. Because of these risks and uncertainties and as a
result of a variety of factors, the actual results, expectations,
achievements or performance may differ materially from those
anticipated and indicated by these forward-looking statements. Any
number of factors could cause actual results to differ materially
from these forward-looking statements as well as future results.
Although Harfang believes that the expectations reflected in
forward-looking statements are reasonable, it can give no
assurances that the expectations of any forward-looking statements
will prove to be correct. Except as required by law, Harfang
disclaims any intention and assumes no obligation to update or
revise any forward-looking statements to reflect actual results,
whether as a result of new information, future events, changes in
assumptions, changes in factors affecting such forward-looking
statements or otherwise.
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.
A photo accompanying this announcement is available at
https://www.globenewswire.com/NewsRoom/AttachmentNg/984e863c-6ccb-48ce-9fdc-6b629e3b3609
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