Float Samples 300m West of the Known Thor Epithermal Deposit Yield Values up to 14.55 g/t Gold and 1,705 g/t Silver, Correspond to EM Targets Upslope From Thor
FOR IMMEDIATE RELEASE
Taranis Resources Inc.
681 Conifer Lane
Estes Park, Colorado
80517
www.taranisresources.com
Float Samples 300m West of the Known Thor Epithermal Deposit Yield Values up to 14.55 g/t
Gold and 1,705 g/t Silver, Correspond to EM Targets Upslope From Thor
Estes Park, Colorado, November 6th, 2023 – Taranis Resources Inc. (“Taranis” or the “Company”)
[TSX.V: TRO, OTCQB: TNREF] is pleased to provide an initial report on exploration conducted in 2023
at Thor. A high -priority electromagnetic (“ EM”) target located over 300m west of the Thor deposit ,
designated ‘Horton’, was evaluated and yielded promising exploration results.
The entirety of the known Thor epithermal deposit occurs east of a major NNW -trending fault called the
Ripper Fault. Horton is the first time any epithermal mineralization has been located west of the Ripper
Fault. Mineralized boulders occur in a field which has been derived from an unknown source up the south
side of Great Northern Mountain. If the source of the Horton boulder field can be located in bedrock , it
means that the epithermal Mineral resource at Thor extends much further to the west than previously known,
and this is graphically shown on a cross-section that can be found on the company’s website.
A map that highlights the features discussed in this News Release is attached, and additional information
can be found at https://www.jjgmining.com/uploads/2/7/0/2/27029932/nr.jpg There are also additional
images including cross-sections and photographs of some of the float samples on the website.
Horton - Geophysical Features
Horton is a circular feature, 600m in diameter visible on airphotos, and is surrounded by a number of EM
anomalies. In May of 2022, an airborne magnetotelluric (“MT”) and magnetic survey completed by Expert
Geophysics (“EG”) confirmed the presence of previously known strong EM-37 anomalies located on the
NW edge of Horton. Data from VLF surveys completed in 2007 further corroborate s the EM-37 and MT
anomalies.
The EG MT survey also identified a large resistive lobe-like feature located to the east of Horton. Taranis
refers to the resistivity feature as “The Claw” owing to its distinctive , hand-like appearance. The Claw is
interpreted to be a buried quartz-rich granitic body and associated silicification that underlies the known
Thor epithermal deposit. Taranis has also been able to locate intrusive rocks at Thor in an old drill hole at
Thor (Thor-210) and in surface prospecting, and this will be discussed in an upcoming News Release.
Ripper Fault and the Gold Pit Knocker
A group of conductive EM-37 anomalies aligned in a north-northwest-trend defines the Ripper Fault that
also delineates the western edge of the known Thor epithermal deposit. In 2022, exposures were made of
this fault and it shows a near-vertical attitude. In several places, the fault includes extremely high-grade
gold and silver mineralization; it appears to be pieces of the Thor epithermal deposit that have been shredded
and incorporated into the Ripper Fault.
Discovery of High-Grade Boulders at Horton
Taranis decided to investigate the conductive geophysical targets and identified a number of mineralized
boulders (some weighing several tons). The boulders are mineralized with quartz-carbonate veining, pyrite,
tetrahedrite, chalcopyrite and sphalerite, and occur topographically higher than the Thor epithermal deposit
making it impossible to have been derived from the known deposit. That said, the origin of these mineralized
boulders has not been located in bedrock as the area has upwards of 95% colluvium/rockslide material
covering bedrock. Taranis completed additional rock, soil, stream sediment and VLF surveys over the area
and the results and interpretation of this exploration work are in progress. The following table shows the
initial eight float samples that were analyzed.
Horton Initial Sample Analyses
(Surface Mineralized Boulders)
Sample
No.
Rock Description Au
(g/t)
Ag
(g/t)
Cd
(ppm)
Cu
(%)
Pb
(%)
Zn
(%)
Sb
(ppm)
S
(%)
3241044 Massive pyrite & tetrahedrite 14.55 1,045 42.7 3.23 0.05 0.43 3.17 43.4
3241045 Quartz/Sediment breccia with
vugging
1.05 292.0 0.9 0.07 0.08 0.01 0.44 0.5
3241046 Banded pyrite with tetrahedrite
clots
3.28 470.0 19.6 1.17 0.28 0.23 0.71 29.7
3241047 Quartz/Sediment breccia with
dodecahedral pyrite (5%) and
early-phase pyrite (10%)
(graphite)
1.88 13.7 0.5 0.03 0.02 0.01 0.02 9.4
3241048 Quartz-Carbonate-sediment
Breccia (FeOx)
0.15 4.9 <0.5 0.02 0.03 0.01 0.01 0.4
3241049 Banded quartz-siderite vein with
5% pyrite, styolitic
0.82 4.2 <0.5 0.00 0.01 0.01 0.00 6.2
3241050 Very weathered, silver-color
sulfide., extensive vugging
6.31 1,705 3.5 0.24 2.40 0.04 0.84 16.3
3241319 FeOx Quartz vein with pyrite
and vugging
0.33 109.0 1.2 0.08 0.01 0.01 0.04 3.0
*Samples in bold are shown in photographs on the website at www.taranisresources.com
Some of the samples from this a rea exhibit brecciate d textures not found in the known Thor deposit ,
including widespread brecciation and massive clots of tetrahedrite in massive sulfide. The metal content is
also notably different from the main Thor deposit, showing enrichment of precious metals , elevated
antimony content and depletion of base metals. It also matches the tenors and metal content of the
mineralization found in Gold Pit - suggesting a geological link between Horton and Gold Pit.
Comment
John Gardiner, President and CEO of Taranis comments , “a big mystery with the epithermal deposit has
been its low length/width ratio – in fact it is 1 :10. If ther e is a downfaulted portion of the deposit to the
west, then that ratio is going to be something more typical like a 1:4 or 1:3 ratio, and much closer to the
ideal un-eroded 1:1 epithermal deposit that formed over an intrusive source. This has obvious consequences
for the size of the Mineral Resource at Thor. In 2024, Taranis hopes to have permits to drill deep holes to
the east of the deposit where we believe there is an intrusive body related to the overlying epithermal
deposit. To be frank, we never followed up on the Horton Target because it was located off-trend from the
main deposit. In hindsight, Horton makes perfect sense in the context of our linked porphyry -epithermal
model of the Thor deposit, and we are very excited to begin systematic exploration of this target”.
Quality Control
Sampling and collection of samples was undertaken and completed by John Gardiner. Float samples from
the Thor Project are shipped to ALS Geochemistry (“ALS”) Kamloops for preparation. Analyses are
completed by ALS in Vancouver, which is accredited to ISO/IEC 17025:2017 general requirements for the
competence of testing and calibration laboratories. Gold is determined using a one-tonne fire assay method,
with an atomic absorption finish. Silver content is determined using Inductively Coupled Plasma
Spectroscopy (“ICP”), and in cases where silver content exceeds 100 ppm, samples are gravimetrically
reanalyzed where over limits are required. The content of other metals is also determined using ICP, and in
cases where the metal content exceeds analytical limits, the sample is analyzed using ICP with a different
set of calibration standards.
Qualified Person
Exploration activities at Thor were overseen by John Gardiner (P. Geo.), who is a Qualified Person under
the meaning of Canadian National Instrument 43-101. Mr. Gardiner is responsible for, and approves of the
technical content in this News Release. John Gardiner is a principal of John J. Gardiner & Associates, LLC
which operates in British Columbia under Firm Permit Number 1002256.
For additional information on Taranis or its 100% -owned Thor project in British Columbia, visit
www.taranisresources.com
Taranis currently has 94,587,027 shares issued and outstanding (109,262,027 shares on a fully -diluted
basis).
TARANIS RESOURCES INC.
Per: John J. Gardiner (P. Geo.),
President and CEO
For further information contact:
John J. Gardiner
681 Conifer Lane
Estes Park, Colorado 80517
Phone: (303) 716-5922 Cell:
(720) 209-3049
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