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Teuton Resources Corp V.TUO

Alternate Symbol(s):  TEUTF

Teuton Resources Corp. is a Canada-based exploration-stage company. The Company is engaged in the business of acquiring, exploring, and dealing in mineral properties in the province of British Columbia, Canada. The Company owns interests in more than thirty properties in the prolific Golden Triangle area of northwestern British Columbia. Its property portfolio includes Treaty Creek Property, Eskay Rift Property, Harry Property, Del Norte Property, Lord Nelson Property, Orion Property, Big Gold Property, Tonga Property, Fiji Property, King Tut Property, Tuck Property, High North Property, Delta Property, Fairweather Property, Tennyson Property, Pearson Property, Clone Property, Four J’s Property, Konkin Silver Property, Midas Property, Bay Silver Property, Bonsai Property, Gold Mountain Property, Ram Property, Silver Leduc Property, Stamp Property, and Treaty East Property.


TSXV:TUO - Post by User

Comment by highperon Jun 07, 2023 1:29am
223 Views
Post# 35483742

RE:RE:RE:RE:NE stepouts

RE:RE:RE:RE:NE stepoutsThe next photo of a short section of the drill core from about 33 meters further down the hole also inspired my speculative fancy. Disseminated chalcopyrite and strong potassic alteration. 

I googled strength of potassic alteration in a porphyry copper deposit and I found "This type of alteration is typically found at the core of porphyry copper deposits.. "

 
 
Potassic alteration involves the formation of new potassium feldspar and/or biotite. There may also be small amounts of sericite, chlorite and quartz. This type of alteration is typically found at the core of porphyry copper deposits and is the result of alteration by very high temperature potassium-rich fluids.Jul 16, 2021
So can i speculate that tudor wanted to say the
porphyry is very strong in the second photo they
presented? The assays will speak for themselves
but the location of this short interval is many meters
from the outlined area of the deposit.

 
""

 
 
Potassic alteration involves the formation of new potassium feldspar and/or biotite. There may also be small amounts of sericite, chlorite and quartz. This type of alteration is typically found at the core of porphyry copper deposits and is the result of alteration by very high temperature potassium-rich fluids.Jul 16, 2021
S

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