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Skarb Exploration Corp.
Summary
| Project: | RDR | |
|---|---|---|
| Deposit: | RDR | |
| Location: | Canada | |
| Commodities: | Gold | |
| Date: | 1/18/2019 | |
| Report Code: | NI43-101 | |
| Report Type: | Supporting Acquisition | |
| Project Stage: | Pursuing Resources Definition | |
| Report details: | 18-1-2019: Skarb Exploration Corp. announces a Supporting Acquisition report for its RDR deposit at the RDR project. Summary of property in support of IPO. At the request of Skarb Exploration Corp. (the “Company”), this Technical Report on the RDR Gold Pr | |
| Resources: | x | |
| CP/QP: | [Overall Report]: Steven Lauzier, Pierre-Alexandre Pelletier (SL Exploration Inc.) | |
| ABSTRACT: | At the request of Skarb Exploration Corp. (the “Company”), this Technical Report on the RDR Gold Project (the “Property”) has been prepared to provide documentation for an Initial Public Offering (“IPO”) and listing on the Canadian Securities Exchange (“CSE”). Location The Property is located approximately 264 km north-east of Val-d’Or in the province of Québec and 10 km south-east of the town of Waswanipi. Access to the Property is achieved by the paved Québec Provincial Highway #113, which runs from the Trans-Canada Highway #117 near the hamlet of Louvicourt to Chibougamau. Commercial flights are available daily from Montreal to Val-d’Or. Description of Property The Property is made up of 16 claims (covering 891.91 ha) and is located within the Abitibi Greenstone Belt (Northwestern Québec, Canada) in the Township of Gand. It lies within NTS sheet 32G12 and the Property’s center point is located at 438,890mE and 5,499,603mN, 10 km south-east of the village of Waswanipi. Geology and Mineralization The Property area overlies the central core of the Abitibi Greenstone Belt within the Superior province. The claims are centered on a north-east band of intermediate tuffs intermixed with sedimentary rocks (volcanic in origin), in contact with a large layered ultramafic complex. The complex is bound to the north by a series of mafic to intermediate volcanic rocks. The contact between the tuffs and the ultramafics is defined by a regional-scale fault, the Lamarck Fault. The region is also cut by several Proterozoic Diabase dykes. The rocks on the Property include mafic to intermediate flows and tuffs of the Obatogamau Formation; The Complexe d’Esturgeon, a large, layered ultramafic complex with carbonatite and mafic to ultramafic sills. The complex is overlain by slivers of the younger Wachibagau Member, composed of felsic to intermedia | |
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