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Fiorentina Minerals Inc.
Summary
| Project: | Consortium | |
|---|---|---|
| Deposit: | Consortium | |
| Location: | Canada | |
| Commodities: | Gold-Silver-Copper | |
| Date: | 5/15/2019 | |
| Report Code: | NI43-101 | |
| Report Type: | Supporting Acquisition | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 15-5-2019: Fiorentina Minerals Inc. announces a Supporting Acquisition report for its Consortium deposit at the Consortium project. Summary of property in support of acquisition. km NW of Campbell River on Vancouver Island, British Columbia. It constitute | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Hardolph Wasteneys (Bravewolf Consulting) | |
| ABSTRACT: | km NW of Campbell River on Vancouver Island, British Columbia. It constitutes 3 contiguous mineral claims numbered 1055533, 1057452 and 1061232 amounting to 1161 hectares in the BC Mineral Title Online cell system which lists Craig Lynes as sole owner of each. The centre of the Property is at 126º0’19” West longitude by 50°03’59” North latitude and in UTM zone 9 at 714317 East by 5550323 N (NAD 83). There are no other adjoining claims. The Consortium claims are NE of the valley of Consort Creek, which drains out of Stewart Lake at an elevation of 500 meters. Steep hillsides lead up into alpine terrane locally as high as 1500 meters to the NE of the claims and characterized by the presence of glacial tarns. The Consortium claims are underlain by Triassic Karmutsen Formation tholeiitic basalts that were deposited as a submarine plateau by fl ood type eruptions. They were deformed slightly from sub-horizontal by brittle faulting and have been intruded by magmas of the Jurassic Island Intrusive Suite, represented a series of largely granodioritic calc-alkaline intrusions in areas within 10 kilometers of the claims and by dykes within the claims. Various Jurassic and possibly younger intrusions, including a Miocene suite, occur in the North Island associated with porphyry deposits, and many fault structures are associated with epigenetic mineralization. | |
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