Torr Metals Generates Multiple Untested Copper-Gold Targets Across 8.5 Kilometres Within the Hu Zone
Torr Metals Generates Multiple Untested
Copper-Gold Targets Across 8.5 Kilometres
Within the Hu Zone
Vancouver, British Columbia--(Newsfile Corp. - November 21, 2022) - Torr Metals Inc. (TSXV: TMET)
("
Torr"
or the "
Company
") is pleased to report on its extensive compilation of 2134 historical soil
samples within the Hu Zone, a significant target area situated in the northwest portion of the Company's
100% owned 689 km
2
Latham Project. The Hu Zone is road-accessible from the Telegraph Creek road
~12 kilometres (km) southwest of Dease Lake, British Columbia, and encompasses two registered
historical copper-gold-molybdenum occurrences at Hu West and Stain Creek (Figure 1). The Latham
Project is situated within a highway-accessible region of the prolific Golden Triangle of northern British
Columbia.
Within the Hu Zone the Company has identified an extensive footprint of >100 ppm copper (Cu)
anomalies distributed along a significant 8.5 km strike-length that parallels the Hu West and
Stain Creek occurrences (Figure 2).
Within this footprint are three high-priority >300 ppm
copper soil anomalies at the Copper Ridge, Huey, and Stain Creek
targets
coincident with
historical soils containing anomalous gold (Au), silver (Ag), molybdenum (Mo), zinc (Zn), and lead (Pb).
Malcolm Dorsey, President and CEO, commented, "Together with Torr's extensive 2022 fieldwork our
efforts to date have been very successful in identifying multiple high-quality kilometre-scale and road-
accessible exploration targets at the Hu, Dalvenie, and Gnat Pass Zones. In addition to the Gnat Pass
copper-gold porphyry deposit there is now excellent potential for major new copper-gold discoveries
within the untested Hu and Dalvenie Zones, which provides significant upside potential as well as a solid
foundation for investigating the remainder of the largely underexplored district-scale Latham Project."
Highlights
Significant geochemical copper soil anomaly footprint measuring ~8.5 km in strike-length
and up to 2.2 km in width
,
with 265 historical soil samples >100 ppm copper, remaining open to
the north and east of Stain Creek (Figure 2).
Highly anomalous historical copper soil anomalies identified at the Copper Ridge, Huey,
and Stain Creek targets
with 31 historical soil samples >300 ppm copper (Figure 2).
Definition of a potential copper-gold porphyry target (Huey Target) defined by a soil
anomaly measuring an approximate 750 metres (m) by 450 m (Figure 2)
, with 20 historical
soil samples >300 ppm copper, coincident with additional anomalous pathfinder elements
including gold (>31 ppb), silver (>1 ppm), molybdenum (>5 ppm), zinc (>150 ppm), lead (>20
ppm), arsenic (>50 ppm), and antimony (>3 ppm). The presence of these pathfinder elements is
suggestive of the upper portions of a porphyry system, with signatures comparable to the
Company's Gnat Pass copper-gold porphyry deposit located ~26 km to the east-southeast.
~8.2 km
2
of coincident historical induced polarization (IP) and ground magnetic
geophysical surveys within the Hu Zone, both of which are currently being reprocessed.
This data will provide for future cost-effective exploration and delineation of potential additional
targets.
Figure 1.
Known mineral occurrences together with high-priority historical soil anomaly targets and
mapped location of highly-prospective Late Triassic to Early Jurassic multiphase intrusions within the Hu
Zone.
To view an enhanced version of Figure 1, please visit:
https://images.newsfilecorp.com/files/6794/144859_528c55b0f48b18c8_001full.jpg
Geology of the Hu Zone
The Hu Zone is situated within Late Triassic Upper Stuhini Group volcanic and sedimentary rocks and
Late Triassic to Early Jurassic monzonite, diorite, and syenite intrusions. This age and type of intrusions
hosted within Upper Stuhini Group rocks is associated with significant copper-gold porphyry deposits
within the region, including the nearby Red Chris and Saddle North deposits
1
, respectively located ~75
km and ~59 km to the southeast and south of the Hu Zone.
Mapping in the Hu area had previously been conducted by the British Columbia Geological Survey, who
identified two regional-scale faults that have been interpreted by Torr to intersect with the Huey Target;
located at the approximated contact between mapped host rocks of Upper Stuhini Group volcanics and
sediments and multi-phase monzonite and diorite intrusions (Figure 2).
A similar geological setting is found to the east of the Huey target at the Stain Creek copper-gold-
molybdenum occurrence (Figure 2), where more abundant rock exposure exhibits extensive potassic
and silica alteration, together with patchy clay-carbonate associated with shear structures. Potassic
alteration at Stain Creek consists of potassium feldspar, epidote, chlorite, magnetite, and biotite, and is
most strongly developed in close proximity to syenite or monzonite intrusive rocks and in areas of
intense fracturing or faulting. These encouraging characteristics are suggestive of proximity to a large-
scale and potentially fertile geological and structural setting at the Huey and Stain Creek targets, which
will be a focus for future follow-up exploration.
Figure 2.
Known mineral occurrences together with high-priority historical soil anomaly targets and
mapped location of highly-prospective Late Triassic to Early Jurassic multiphase intrusions within the Hu
Zone.
To view an enhanced version of Figure 2, please visit:
https://images.newsfilecorp.com/files/6794/144859_528c55b0f48b18c8_002full.jpg
1
2012 Technical Report on the Red Chris Copper-Gold Project, February 14, 2012. NI 43-101 Technical Report on the Saddle North Copper-Gold
Project, Tatogga Property, August 20, 2020.
Exploration Update
Dalvenie Zone induced polarization (IP) survey has been completed and currently undergoing
processing.
Assays pending on 275 rock grab samples and 1316 soil samples collected during the 2022 field
program.
Qualified Person
The technical content of this news release has been reviewed and approved by Michael Dufresne,
M.Sc., P.Geol., P.Geo., a consultant to the Company who is a qualified person defined under National
Instrument 43-101.
About Torr Metals
Torr Metals is a Vancouver based mineral exploration company focused on defining and developing the
substantial exploration and resource potential of the ~689 km
2
Latham Copper-Gold Project, located
within the prolific Golden Triangle of northern British Columbia. Year-round access is provided by
Highway 37 with the project being favourably located 16 km south of the regional airport in Dease Lake.
For further details about the Latham Copper-Gold Project, please refer to the Company's website or
current geological Technical Report (August 24, 2021) filed on November 25, 2021 under the
Company's profile on SEDAR at
www.sedar.com
.
On behalf of the Board of Directors
Torr Metals Inc.
"Malcolm Dorsey"
Malcolm Dorsey
President, CEO and Director
For further information:
Malcolm Dorsey
Telephone: 236-982-4300
Email:
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Exchange) accepts responsibility for the adequacy or accuracy of this press release.
Cautionary Statement Regarding Forward-Looking Information
This press release contains "forward-looking information" within the meaning of applicable Canadian securities legislation. Forward-looking
information includes, without limitation, statements regarding the use of proceeds from the Company's recently completed financings, and the
future plans or prospects of the Company. Generally, forward-looking information can be identified by the use of forward-looking terminology such
as "plans", "expects" or "does not expect", "is expected", "budget", "scheduled", "estimates", "forecasts", "intends", "anticipates" or "does not
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"will be taken", "occur" or "be achieved". Forward-looking statements are necessarily based upon a number of assumptions that, while considered
reasonable by management, are inherently subject to business, market and economic risks, uncertainties and contingencies that may cause
actual results, performance or achievements to be materially different from those expressed or implied by forward-looking statements. Although
the Company has attempted to identify important factors that could cause actual results to differ materially from those contained in forward-looking
information, there may be other factors that cause results not to be as anticipated, estimated or intended. There can be no assurance that such
information will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements.
Accordingly, readers should not place undue reliance on forward-looking information. Other factors which could materially affect such forward-
looking information are described in the risk factors in the Company's most recent annual management's discussion and analysis which is
available on the Company's profile on SEDAR at
www.sedar.com
. The Company does not undertake to update any forward-looking information,
except in accordance with applicable securities laws.
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