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Taranis Resources Inc V.TRO

Alternate Symbol(s):  TNREF

Taranis Resources Inc. is a mineral exploration company. The Company is principally engaged in the acquisition, exploration and development of precious and base metal projects. The Company owns a 100% interest in certain mineral rights entitled the Thor Property located in the Revelstoke Mining District of British Columbia, Canada and holds certain contiguous mineral claims. It has drilled over 250 drill holes on the project, defining a near-surface epithermal deposit that is over 2 km long. The Thor project is a collection of over 27 Crown Granted Mineral Claims and approximately 14 Mineral Tenures covering approximately 3,314 hectares, which forms a contiguous property over the Thor precious and base metal Deposit. The Company, together with its subsidiaries, is engaged in acquiring and exploring its mineral properties.


TSXV:TRO - Post by User

Post by TrumpThison Feb 17, 2023 12:24pm
190 Views
Post# 35292308

THOR Project in 3D - #2 E-W Cross Section

THOR Project in 3D - #2 E-W Cross Section on Feb 14 I posted about the Horizontal Section, now I'm bringing to light the East-West Cross Section from TaranisResources website. I'm not a geo, just an active investor, glad TRO had Expert Geophysics do a MobileMT survey (internally funded) & I find the detail amazing with comparisons to other mining camps, a compeling investment reason, and can't wait until the curtain is pulled back on the porphyry intrusion after the deep drill this summer:

EAST-WEST CROSS SECTION

The airborne MT survey was able to identify a large conductivity 'donut' that lies under the Thor epithermal deposit. In the image to the left, a slice is taken through the geophysical data that shows this feature. The intrusive 'donut' is overlain very silicified rocks of the Broadview Formation, and this forms a plug-like feature over the donut. This area is known to contain very silicified rocks of the Broadview Formation which are suspected to occur on the apex of an underlying intrusive body that occurs in the conductivity 'donut'.

The limited shallow drilling in this area has encountered great widths (over several hundred meters) of sericite and andalusite alteration. In this model, the intrusion is seen as the source of metals that formed the Thor epithermal deposit from a much deeper intrusive body.
Picture
East - West Cross Section through the epithermal deposit on section 5,616,700 North graphically demonstrating the intrusive-related 'donut' feature under the epithermal deposit and the resistive 'plug' centered on top of the feature.

GLTA that are backing up the truck!
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