Torr Identifies 6 New Gold Bearing Structures With Soil Samples Up to 1.32 g/t Au on the Filion Project
Torr Identifies 6 New Gold Bearing Structures
With Soil Samples Up to 1.32 g/t Au on the
Filion Project
Vancouver, British Columbia--(Newsfile Corp. - January 15, 2024) - Torr Metals Inc. (TSXV: TMET)
("
Torr"
or the "
Company
") is pleased to announce the identification of multiple new gold (Au)
anomalies in humus soil sampling with
assays yielding up to 1.32 g/t Au that have never been drill
tested
. The soil anomalies occur coincident with six kilometre-scale VLF-EM (very low frequency
electromagnetic) conductors interpreted as significant shear structures with northeast-southwest and
east-west orientations that occur within a >7 kilometre (km) dilational bend of the Filion Fault, defined by
a break in the linear east-west trending high magnetic signature associated with magnetically
susceptible stratigraphy (Figure 1, Figure 2). Fieldwork in 2023 also confirmed in localized outcrop that
VLF-EM conductors and soil anomalies occur coincident with highly prospective stratigraphic contact
zones for gold endowment, including mafic volcanics and quartz-feldspar porphyry that account for the
underlying linear moderate to high and flanking low magnetic anomalies respectively (Figure 2).
Within the regional greenstone belts of northern Ontario early syn-volcanic aged gold deposits (Figure 3;
including Hemlo, Greenstone, Casa Berardi, Detour Lake) are commonly found within major east-west
trending deformation zones with a similar setting to the Filion Fault with chief emplacement controls for
gold consisting of dilational bends as well as competency contrasts along major stratigraphic contacts.
Both of these characteristics have now been identified on the Filion Project together with coincident
VLF-EM conductors and gold soil anomalies that remain open in all directions and untested by drilling.
The 100% owned Filion Gold Project (the "Project") is located within a prolific region of northern Ontario
that hosts a number of major gold mine producers with deposits occurring in comparable geological
settings (Figure 3). The Project is ideally situated adjacent to excellent infrastructure with the town of
Kapuskasing located ~30 km to the southeast and direct road access 4 km from the Trans-Canada
Highway, regional railway, and provincial power grid.
Highlights Include:
2023 humus soil samples detected multiple
gold (Au) soil anomalies
coincident with 6 historical
VLF-EM conductors across a
structural corridor measuring greater than 2.5 km in width
. Of
318 humus soil samples collected 39 yielded >10 ppb Au, with 13 samples >20 ppb Au up to
1,320 ppb Au.
The 1,320 ppb Au soil sample was collected in proximity to a historical
trench
where historical channel sampling reportedly yielded 91.4 g/t Au over 0.3 metres
(m)
1
(Figure 2).
Humus soil sampling along the interpreted Filion Fault indicates
anomalous gold along a ~1200
metre strike-length
along-trend of the Oscar occurrence, where a
historical rock grab sample
assayed 9.1 g/t Au
2
.
These results
define a significant extension to this portion of the
mineralizing system that now measures 2.5 km in strike-length
(Figure 2).
No soil anomalies >20 ppb Au have ever been drill tested
and
more than 75% of the highly
prospective 28 conductors
located within the >7 km dilational bend in the Filion Fault remain
untested by humus soil sampling (Figure 2).
Mineralization becomes more robust in grade and distribution where east-west trending
conductors (numbered 4-6, Figure 2) are concentrated along the interpreted Filion Fault; where
significant shear systems were observed in outcrop together with extensive arsenopyrite-pyrite
mineralization within quartz-carbonate stockwork and veining that is also host to chlorite-sericite-
silica-fuchsite alteration, characteristics that in other regions of Ontario yield significant gold
deposits.
Torr is currently in the process of applying for a drill permit to test these targets
in 2024.
Malcolm Dorsey, President and CEO, commented, "These are fantastic results from our preliminary
reconnaissance work that is a proof of concept to our exploration model; supporting our interpretation
that the geological setting of the Filion Fault is similar to other well known gold endowed regional
structures that are host to major deposits in northern Ontario. We are very encouraged by the apparent
robust nature of the mineralization where multiple paralleling shear structures are more concentrated
along the Filion Fault, providing an excellent exploration target with scalability adjacent to the Trans-
Canada Highway. This is a rare ground-floor opportunity for major new discovery potential, which we will
be excitedly looking to further advance with drilling in 2024."
Figure 1.
Filion Project location with underlying 1
st
derivative airborne magnetic geophysics at 200 m
line spacing (Source: Canadian and Ontario Geological Surveys) annotated with historical gold
occurrences, rock grab sampling, and structural interpretation.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6794/194202_d30235bbb48a8bbf_001full.jpg
Figure 2.
Filion West displaying location of anomalous gold in 2023 humus soil samples and 1985 VLF-
EM conductors coincident with linear moderate to high magnetic signatures from airborne geophysics.
Conductors occur within a highly prospective >7 km dilational bend of the Filion Fault, resulting in a
"break" in the east-west trending high magnetic (iron formation) signature.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6794/194202_d30235bbb48a8bbf_002full.jpg
Humus Soil Sampling Results Discussion:
Field mapping of rare outcrop in 2023 confirmed the historically-reported host lithologies as well as
styles of alteration and mineralization that identifies the Filion Project as an area conducive to gold
endowment, that with a thin veneer of till cover is also an ideal setting for humus soil sampling methods.
The 2023 Filion Project humus soil sampling results were highly anomalous for coincident gold
(predominantly ranging from 5 to 1,320 ppb Au), arsenic (2 to 65 ppm), and molybdenum (1 to 4 ppm).
Arsenic (As) and molybdenum (Mo) are considered indicators for gold mineralization in humus sampling
over thin till overburden at the Williams Gold Mine, part of the Hemlo Mining Camp (Figure 3); where
previous studies yielded gold from 2 to 75 ppb, arsenic from 4 to 12 ppm, and molybdenum from 0.5 to
3.7 ppm; higher values correlated to known mineralized gold zone trends identified in outcrop
4
.
Historical Drill Hole DH 88-7
With the first soil sampling survey ever conducted on the Project area in its maiden 2023 field program
Torr also confirmed that the majority of historical drilling activity did not test the most prospective
mineralized trends or shear structure conductors. Only the historical drill hole DH 88-7 appears to have
intercepted a priority conductor (labelled #2 in Figure 2) along-trend of anomalous gold in 2023 humus
sampling. Although no assays are provided in the historical record the core logs for DH 88-7 describe
quartz veining associated with variable amounts of pyrite-arsenopyrite mineralization and silica-sericite-
tourmaline alteration hosted by metasediments and mafic metavolcanics from 16.7 metres to the end of
hole at 89.9 metres, with veining and alteration being concentrated along the contacts between those
units and an interbedded quartz-feldspar porphyry. Within this interval a section from 49.4 metres to 60.3
metres contained extensive quartz veining with moderate to strong silicification and sericitization
together with enhanced pyrite-arsenopyrite mineralization. This style of strong hydrothermal alteration
and mineralization along-trend of anomalous 2023 humus sampling indicates potential for significant
mineralized intervals associated with identified conductors that will provide Torr with multiple highly
prospective exploration targets in 2024.
Figure 3.
Filion Project location within the prolific gold-endowed greenstone belts of the Wabigoon,
Wawa, and Abitibi subprovinces of northern Ontario. Figure includes the positions as well as total
historical and forecasted production of major regional gold mines.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6794/194202_d30235bbb48a8bbf_003full.jpg
1
Residen
t Geologist files T-0223, Timmins RGP office, certificate unavailable.
2
Luhta, L. 1985. Ontario Ministry of Natural Resources, Timmins. Resident Geologist files T-0201.
3
Comparisons disclosed are not necessarily indicative of mineralization on the Filion Gold Project.
4
Fortescue, JAC. 1985. A Standardized Approach to the Study of the Geochemistry of Humus, Williams Property, Hemlo, Thunder Bay District.
Ontario Geological Survey. Map 80 716. Geochemical Series. Compiled 1985.
Methodology and QA/QC
The analytical work reported on herein was performed by ALS which is a ISO-IEC 17025:2017 and ISO
9001:2015 accredited Geoanalytical laboratory.
Humus soil samples were subject to screening at 180 microns, and analysis of a 0.5 gram sample
digested in aqua-regia via multi-element ICP-MS (ME-MS41) and gold via a fire-assay atomic
absorption (FA-AA) finish (Au-AA23). Rock channel and grab samples were crushed to 70% passing
<2mm followed by pulverization of a 250 gram sample split to 85% passing 75 microns and analyzed for
34 elements in a four acid digestion via-multi-element ICP-AES (ME-ICP61) and for gold via a FA-AA
finish (Au-AA23). The Company follows industry standard procedures for the work carried out on the
Filion Project. Given the reconnaissance nature of the samples submitted (select rock grab and humus
soil sampling) the Company has relied on the internal quality assurance/quality control (QA/QC)
measures of ALS. In addition, 1 in 20 humus soil samples were collected in duplicate to assess
repeatability. Torr Metals detected no significant QA/QC issues during review of the data.
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 potential of its 100% owned portfolio of district-scale gold and copper projects;
including the ~261 km
2
Filion Gold Project in northern Ontario, ~140 km
2
Kolos Copper-Gold Project in
south-central British Columbia, and ~689 km
2
Latham Copper-Gold Project which includes the Gnat
Pass deposit in northern British Columbia. All projects are located in prolific mining regions with
substantial infrastructure and favourable geology for significant new discovery potential. For further
details please refer to the Company's website or geological Technical Reports (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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