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Lodge Resources Inc.
Summary
| Project: | Comstock | |
|---|---|---|
| Deposit: | Comstock | |
| Location: | Canada | |
| Commodities: | Gold-Silver-Lead-Zinc-Copper | |
| Date: | 8/19/2019 | |
| Report Code: | NI43-101 | |
| Report Type: | Supporting Acquisition | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 19-8-2019: Lodge Resources Inc. announces a Supporting Acquisition report for its Comstock deposit at the Comstock project. Amended and restated report - summary of property in support of acquisition. Lodge Minerals Inc., a wholly owned subsidiary of Lodg | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Laurence Sookochoff (Sookochoff Consultants Inc.) | |
| ABSTRACT: | Lodge Minerals Inc., a wholly owned subsidiary of Lodge Resources Inc., is the optionee of the contiguous 12 claim 664 hectare Comstock property ("Property") located within the Nicola Mining District of south-central British Columbia. The Property is located within the regional Quesnel Trough, a 30 to 60, km wide belt of Lower Mesozoic volcanic and related strata stretching from the US border in the south to the northern British Columbia border, and is a belt of producing and past productive porphyry copper mineral deposits. The Comstock property is located within this Belt between two producing mines; the Copper Mountain porphyry copper-gold mine 80 kilometres to the south with a reported production of 40,000 tonnes per day; and Canada's largest mine, the Highland Valley Copper mine 53 kilometres northwest with a reported production of 147,000 tonnes per day. The Comstock property is underlain by the Nicola Western Belt of flow and pyroclastic rocks ranging in composition from andesite to rhyolite with interbedded limestone, volcanic conglomerate, and sandstone. Of the seven designated mineral areas, one main mineral area is a volcanogenic sulphide (VMS) within a two kilometre, northeasterly trending rhyolite/pyroclastic flow which hosts the LD and the Comstock volcanogenic massive sulphide (VMS) mineral showings. The second main area of mineralization is a zone of mineral bearing quartz veins within a 2,800 metre northwesterly trending structure hosting the Charmer and Diane mineral zones. Since 1896 when shafts were sunk on three copper-iron showings, exploration has progressively continued continued to 2018 on ground covered by the Comstock property The exploration was successful in the determination of two main mineral zones over significant lengths with a discontinuous and/or continuous exposure over limited lengths. | |
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