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Taranis Resources Inc. V.TRO

Alternate Symbol(s):  TNREF

Metals & Mining Industrial Metals & Minerals
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

Taranis Resources Inc.
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Post by TrumpThison Sep 06, 2024 6:45pm
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Post# 36212660

THOR has a proven Epithermal system & drilling the Porphyry!

THOR has a proven Epithermal system & drilling the Porphyry!Skip Nav Destination
The porphyry is the source of the Lepanto epithermal system and is connected to it deep within the earth. It turns out that this main course contains at least 25 times the tonnage of Lepanto and today that's worth nearly $80 billion.

Research Article| November 01, 2022

High-Grade Copper and Gold Deposited During Postpotassic Chlorite-White Mica-Albite Stage in the Far Southeast Porphyry Deposit, Philippines 

https://pubs.geoscienceworld.org/segweb/economicgeology/article/117/7/1573/617513/High-Grade-Copper-and-Gold-Deposited-During
A. Geologic map of the Mankayan district showing volcanic units (modified from Chang et al., 2011). The surface projection of the Lepanto high-sulfidation (HS) epithermal, Far Southeast (FSE) porphyry, and intermediate-sulfidation Victoria veins are shown. A 6-km longitudinal section across the district is shown by dashed line, turning north-south to be a cross section in the vicinity of the Victoria veins (Fig. 1B). PRS 92 UTM grid datum. B. Schematic northwest-southeast, north-south long and cross section through the Lepanto enargite-Au high-sulfidation epithermal deposit, the FSE porphyry deposit, and the intermediate-sulfidation Victoria veins (see trace in Fig. 1A; Chang et al., 2011).
A. Geologic map of the Mankayan district showing volcanic units (modified from Chang et al., 2011). The surface projection of the Lepanto high-sulfidation (HS) epithermal, Far Southeast (FSE) porphyry, and intermediate-sulfidation Victoria veins are shown. A 6-km longitudinal section across the district is shown by dashed line, turning north-south to be a cross section in the vicinity of the Victoria veins (Fig. 1B). PRS 92 UTM grid datum. B. Schematic northwest-southeast, north-south long and cross section through the Lepanto enargite-Au high-sulfidation epithermal deposit, the FSE porphyry deposit, and the intermediate-sulfidation Victoria veins (see trace in Fig. 1A; Chang et al., 2011).
https://www.researchgate.net/figure/Simplified-NW-SE-longitudinal-section-through-the-Lepanto-and-Far-Southeast-FSE_fig3_315344797
Simplified NW-SE longitudinal section through the Lepanto and Far Southeast (FSE) deposits, approximately in the plane of the Lepanto fault (Fig. 1). The approximate extent of enargite-Au ore in the Lepanto deposit, which is largely hosted by silicic alteration with a halo of quartz-alunite, is shown (Garcia, 1991). This lithocap alteration follows the contact of the Imbanguila Fm with the basement volcaniclastic rocks. The location of the samples from the Lepanto underground mine (Appendix Table A1) are plotted on the 680 to 1150 m elevation levels, with other samples from the FSE ore body collected from underground drill holes. The S-isotopic values of stage 1 and 2 sulfide and sulfate minerals are also plotted. Section modified from Concepcin and Cinco (1989) and Garcia (1991). The gold and copper grade shells of the FSE deposit are from Gaibor et al. (2013), projected on to the section. Sample points with sample identifier but no sulfur isotope results are shown to provide spatial reference locations (see Fig. 9 for associated analytical data, such as enargite-hosted fluid inclusion homogenization temperatures).
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