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Alexandria Minerals Corp.
Summary
| Project: | Sleepy Lake | |
|---|---|---|
| Deposit: | Sleepy Lake | |
| Location: | Canada | |
| Commodities: | Gold | |
| Date: | 12/3/2014 | |
| Report Code: | NI43-101 | |
| Report Type: | Resource Estimation | |
| Project Stage: | Pursuing Resource Increase/Upgrade | |
| Report details: | 3-12-2014: Alexandria Minerals Corp. announces a Resource Estimation report for its Sleepy Lake deposit at the Sleepy Lake project. Updated mineral resource estimate for Sleepy Lake project. At the request of Mr. Eric Owens, President of Alexandria Minera | |
| Resources: | (Resource, Inf.): 1.855Mt @ 4.7g/t Au for 279760oz Au contained at Sleepy Lake | |
| CP/QP: | [Resources]: Christian D'Armours (Geopointcom) | |
| ABSTRACT: | At the request of Mr. Eric Owens, President of Alexandria Minerals Corporation (“Alexandria”) Geologica Groupe-Conseil Inc. (“Geologica”) and Mr. Christian D’Amours, P. Geo., from GeoPointCom Inc. were given the mandate to prepare an updated NI 43- 101 Technical Report with resource calculation on the Sleepy Lake Property (“Property”), located in the Abitibi Region of Quebec. On July 17th, 2014 one of the authors, Mr. Alain-Jean Beauregard, collected forty seven (47) core samples in three (3) recent diamond drill holes (SAX-13-025, SAX-14- 027 and SAX-14-028) for analytical testing and data corroboration. A property visit was carried out subsequently on August 8, 2014. The Property is located in the South-central portion of the Abitibi Greenstone Belt, which forms part of the Superior Structural Province. All the rocks of the area are Archean in age, except for NE-striking diabase dykes, which are Proterozoic in age. Volcanic rocks of the Malartic and Piché Groups predominate in the northern half of the area, while clastic sedimentary rocks of the Cadillac and Pontiac Groups are dominant in the southern half of the area. The Sleepy Property is located approximately 2 km north of the Cadillac Break, the most prominent structural feature of the area (also known as the Cadillac Tectonic Zone (‘CTZ’)). The Cadillac Break is located near the contact between the Pontiac Group and the Malartic Group. It is a major tectonic zone that is characterized by intense shearing and mechanical deformation, and it can be traced from West to East over a total distance of approximately 210 kilometers from Kirkland Lake, Ontario in the west, to east of Louvicourt, Quebec. Later conjugate faulting and fracturing of both northeast and, to a lesser extent, northwest trends have also occurred along its length. | |
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