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Stuhini Exploration Ltd.
Summary
| Project: | Metla | |
|---|---|---|
| Deposit: | Metla | |
| Location: | Canada | |
| Commodities: | Gold-Copper | |
| Date: | 12/5/2018 | |
| Report Code: | NI43-101 | |
| Report Type: | Supporting Acquisition | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 5-12-2018: Stuhini Exploration Ltd. announces a Supporting Acquisition report for its Metla deposit at the Metla project. Summary of Metla property. The Metla property is a gold-silver-base metal prospect located in the Chechilda Range of the Coast | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Andrew Wilkins (Lithos Geological Inc.) | |
| ABSTRACT: | The Metla property is a gold-silver-base metal prospect located in the Chechilda Range of the Coast Mountains in northwestern British Columbia. It is approximately 150 km south of town of Atlin and 150 km west of the town of Dease Lake. The property is centred at 58°22’ north latitude and -132°35’ west longitude. Access to the property is by helicopter from Atlin or Dease Lake. The Metla property consists of 7 contiguous mineral claims and covers an area of 6,457.33 hectares. The claims are 100 percent owned by Stuhini Exploration Ltd. of Vancouver, B.C. Regionally, the property straddles the contact between the Jurassic quartz diorite of the Coast Plutonic Complex to the southwest and the sedimentary Palaeozoic to Lower Triassic Stikine Assemblage and Upper Triassic Stuhini Group volcano-sedimentary rocks to the northeast. These rocks are intruded by Late Cretaceous or Paleocene granite to felsic plugs of the Windy Table Suite. The Windy Table Suit is considered part of the Taku River-Trapper Lake-Tatsamenie Lake Cretaceous continental arc volcanoplutonic belt. On the property, northwest trending steep easterly dipping massive andesitic volcanic rocks are underlain by an interbedded series of andesite, pyritic mudstone, impure limestone and calcareous sediments. Extensive areas of phreatic or hydrothermal vent breccia occur cross cutting the volcanic and sedimentary rocks. The breccia is aligned in a northwesterly trending zone 800 metres wide by 2000 metres in length. The breccia consists of an iron rich pyritic carbonate matrix supporting clasts of volcanics, sediments and rarely sulphide (Mawer, 1989). | |
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