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WestKam Gold Corp.
Summary
| Project: | Bonaparte | |
|---|---|---|
| Deposit: | Bonaparte | |
| Location: | Canada | |
| Commodities: | Gold-Silver-Copper-Tellurium | |
| Date: | 8/14/2019 | |
| Report Code: | NI43-101 | |
| Report Type: | Exploration/Drilling Update | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 14-8-2019: WestKam Gold Corp. announces an Exploration/Drilling Update report for its Bonaparte deposit at the Bonaparte project. Technical Report summarising property. The author was retained by WestKam Gold Corp. to complete this report on the Bonaparte | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Rick Kemp (Coast Mountain Geological Ltd.) | |
| ABSTRACT: | The author was retained by WestKam Gold Corp. to complete this report on the Bonaparte Gold project located in south central British Columbia. The purpose of this report is to summarize the work completed on the property, to make recommendations for further work, and to provide a Technical Report that conforms to the format and content standards of National Instrument 43- 101, Companion Policy 43-101CP and Form 43-101F1. This technical report is written for filing purposes on the Canadian Securities Exchange. The 2,461.35-hectare Bonaparte Gold Project is located on NTS map sheet O92P/1W and 092I/16W and is centered at a latitude of 50°59’38.61” N and a longitude of 120°26’11.29” W, approximately 50km to the north northwest of Kamloops BC. The Bonaparte Project, consisting of eight (8) contiguous mining claims within the Kamloops Mining Division is owned 100% by WestKam Gold Corp. The property is road accessible from Kamloops. The stratigraphy exposed on the property consists of a dark, rusty weathering and polydeformed argillaceous sedimentary rocks of the Harper Ranch Group. The Harper Ranch Group of rocks were hornfelsed during the emplacement of a composite quartz diorite to monzodiorite porphyritic intrusion and dike complex. At the Discovery Zone, there are at least three discreet intrusive phases which have been exposed by trenching, drilling and underground development ie a mafic quartz diorite, monzodiorite and aplite. All are overprinted by late hydrothermal quartz and quartz carbonate veining. The monzodiorite is the oldest plutonic phase exposed on the property and is white to pinkish grey on the weathered surface and greenish grey on a fresh surface. The unit is medium grained with 10% biotite as books and replacements of hornblende. Hornblende and K-feldspar occur as sparse outsized crystals up to 1cm long. Chloritized mafic xenoliths are common. The Mafic Quartz Diorite is pervasively biotite altered, well foliated and lineated and hosts disseminated chalcopyrite. Typically, the unit is coarse grained and hosts white plagioclase, altered hornblende and distinctive, sparse blue quartz eyes in a fine-grained matrix. | |
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