Torr Metals Returns High-Grade Rock Samples Within Newly Defined 1200 by 1500 Metre Zone of Cluster Porphyry Targets at Stain Creek
Torr Metals Returns High-Grade Rock Samples
Within Newly Defined 1200 by 1500 Metre Zone
of Cluster Porphyry Targets at Stain Creek
Vancouver, British Columbia--(Newsfile Corp. - April 19, 2023) - Torr Metals Inc. (TSXV: TMET) ("
Torr"
or the "
Company
") is pleased to provide assay results from 30 rock grab samples collected during the
2022 field program that have
extended surface copper (Cu) - gold (Au) - molybdenum (Mo)
mineralization from 300 metres (m) to 575 m at its Stain Creek porphyry target
, which remains
open in all directions (Figure 1). Furthermore, newly reprocessed geophysical data covering 3.7 square
kilometres (km
2
) has outlined
five significant high magnetic anomalies with the potential
for
clustered
porphyry-style targets, some of which are coincident with known surface Cu-Au-Mo
mineralization
(Figure 2). The Stain Creek copper-gold porphyry exploration target is located in the
eastern portion of the 8.5 km multi-target Hu Zone, within the Company's 100% owned 689 km
2
Latham
Project in British Columbia's prolific Golden Triangle. The Stain Creek target is road accessible ~27 km
southwest of the town and regional airport of Dease Lake.
Highlights
Rock grab samples from 2022 have
extended the known Cu-Au-Mo mineralized trend
at
surface
by approximately 275 m. Highlights include:
30 rock grab samples collected in 2022:
5 samples assayed >0.2 grams per tonne (g/t)
Au, 6 samples >0.12% Cu, and 3 samples >15 parts per million (ppm) Mo
.
An approximate
160 m extension to the southeast
within
pervasively altered Stuhini
Group volcanic and sedimentary rocks
with rock grab samples yielding up to
1.55% Cu,
3.28 g/t Au, and 497 ppm Mo
.
Rock grab samples yielding up to
1.59 g/t Au and 19.95 ppm Mo within a strongly
altered syenite intrusion,
extending the mineralized trend by ~115 m to the
northwest
.
Lineaments observed in geophysical data indicate the presence of northwest and northeast-
trending structures with
northwest and east-west controls on the orientation of highly
prospective geophysical anomalies
, the latter being comparable orientations to controls on
mineralization observed at the nearby Red Chris and Saddle North copper-gold porphyry
deposits
1
.
The Stain Creek target has never been drilled; the
coinciding km-scale copper soil anomalies
(see news release from
Jan. 24
th
, 2023
)
, high-grade Cu ± Au ± Mo rock grab samples, and
extensive high magnetic geophysical signatures
make Stain Creek a
priority target for
further exploration in 2023
.
Malcolm Dorsey, President and CEO, commented, "These latest results have greatly advanced the Stain
Creek mineralized trend as a primary undrilled exploration target, alongside our Dalvenie copper-gold
trend. At Stain Creek, within the Hu Zone, we are seeing elevated copper, gold, and molybdenum
coincident with highly magnetic geophysical anomalies that together with styles of mineralization at-
surface form a very compelling potential porphyry cluster target across a significant 1200 m by 1500 m
extent. We are also encouraged by results to date that have indicated a geological setting consistent
with and similar to the Saddle North and Red Chris porphyry deposits, currently being advanced by
majors ~60 km and ~75 km to the south of Stain Creek. With mineralization remaining open in all
directions we are looking forward to further advancing the Stain Creek exploration target in 2023."
Figure 1.
Select rock grab samples and compiled mapping from the Stain Creek target, within the
eastern portion of the Hu Zone.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6794/162952_43e8b727e45ad974_001full.jpg
Figure 2.
Reprocessed historical ground magnetic data showing the locations of rock grab samples,
interpreted structural features, and high priority geophysical targets.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6794/162952_43e8b727e45ad974_002full.jpg
Geological Discussion
Stain Creek is a high priority target characterized by km-scale surface expressions of hydrothermal
alteration and anomalous copper-in-soil. High grade Cu, Au, and Mo mineralization delineates an
approximate 575 m trend to mineralization that remains open for further testing. Gold mineralization at
Stain Creek is associated with potassic alteration concentrated along fractures and faults, while copper
and molybdenum mineralization is associated with brittle-shear-hosted quartz-iron-carbonate veining.
There is significant evidence to suggest a strong structural control to mineralization present at Stain
Creek.
The structural framework of Stain Creek, interpreted from both field mapping and magnetic lineaments,
indicates strong northwest, northeast, and east-west orientations on the geometry of intrusions,
alteration, faulting, and veining. The presence of a large-scale, through-going northwest-oriented
structure is similar to that which hosts mineralization at the Saddle North copper-gold porphyry deposit
located ~60 km to the south-southeast, while east-west trending structures commonly host mineralization
at the Red Chis copper-gold mine, located approximately 75 km in the same direction
1
. Furthermore, the
Late Triassic to Middle Jurassic polyphasic, dioritic to monzonitic to syenitic intrusions present at Stain
Creek are comparable in age, composition, and orientation to the Red Suite, which is the host to
copper-gold porphyry-style mineralization at Red Chris and Saddle North
2
.
Each of the five notable geophysical anomalies at Stain Creek are characterized by magnetic highs that
are partially to completely enveloped by a lower magnetic signature. This setting is comparable to the
porphyry systems at the Company's Gnat Pass copper-gold porphyry deposit, where the magnetite-
bearing mineralized core is surrounded by a halo of magnetically destructive silica alteration and fault
contacts causing the lower magnetic signature. The strongest high magnetic anomalies are interpreted
as an underlying hornblende-biotite monzonite or diorite mass, with narrower signatures likely attributed
to observed syenites or dyke-like extensions of the diorite. As such, the presence of multiple high
magnetic anomalies of highly prospective intrusive compositions coincident or marginal to porphyry-style
Cu-Au-Mo mineralization and alteration suggests significant potential for a substantial cluster porphyry
system concentrated within the Stain Creek area. With an extensive and highly prospective 1200 m by
1500 m geophysical footprint the Stain Creek target area is approximately twice the size of the Gnat
Pass copper-gold porphyry footprint, located ~28 km to the northeast of the Hu Zone.
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.
2
Dease Lake-Little Tuya River Geology (NTS 104J/08, 07E), BC Ministry of Energy and Mines Open File 2012-04 and Geoscience BC Map 2112-08-1.
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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. The Company does not undertake to update any
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