Teuton Resources Corp V.TUO

Alternate Symbol(s): TEUTF

Metals & Mining Industrial Metals & Minerals

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.

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Teuton Resources Corp

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Post by highperon Nov 30, 2020 3:31pm

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Post# 32002521

rhyolite and chlorite - well-defined quartz/carbonate veins

Neighboring property hits rhyolite chlorite high grade veins .... decade is obviously in the right neighborhood but let's wait for the assays...

It was interesting that ovensek's team associated the chlorite with the possibility of of a porphyry being proximate..

On the 14 oz zone the core pictured showed the presence of massive amounts of chlorite and ... while just over a kilometer and a half or so a potential porphyry was mapped by the del norte ztem survey.... lots of thyolite was observed in relation to the area of interest in vicinity of where decade drilled as well...

what it all mean... it is boring waiting for the assays to be reported I suppose

Prospecting has shown that both the Yellow Bowl and VMS Zones are covered by a mafic unit consisting of basalt flows and volcaniclastics which overlie interbedded rhyolite and andesitic volcanics. The zones are marked by intense QSP alteration surrounded by chlorite alteration, believed to be related to a porphyry system at depth. Mineralization intersected to date consists of semi-massive amounts of chalcopyrite, pyrite and locally sphalerite, within well-defined quartz/carbonate veins. These veins were intersected within the upper mafic unit and showed strong alteration of the wall rock and grades improving with depth. This relationship is expected to continue to depth where the veins cut through the underlying andesite/rhyolite volcanics, which experience has shown are better host rocks as seen elsewhere on the property at the Fall Creek, Ice Creek and South zones, as well as in the district as a whole.

https://p2gold.com/news-releases/p2-gold-intersects-high-grade-copper-at-todd-creek-2060/