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Alacer Gold Corp.
Summary
| Project: | Gediktepe | |
|---|---|---|
| Deposit: | Gediktepe | |
| Location: | Turkey | |
| Commodities: | Gold-Silver-Copper-Zinc | |
| Date: | 4/3/2019 | |
| Report Code: | NI43-101 | |
| Report Type: | Feasibility Study | |
| Project Stage: | Pursuing Resource Increase/Upgrade | |
| Report details: | 3-4-2019: Alacer Gold Corp. announces a Feasibility Study report for its Gediktepe deposit at the Gediktepe project. Amended previous Feasibility study to fix a typo. The Gediktepe project is located within the Afyon tectonic zone, which is one of the mai | |
| Resources: | (Reserve, P+P): 18.58Mt @ 0.85g/t Au, 31.8g/t Ag, 0.92% Cu, 1.98% Zn in the Sulphide Zone | |
| CP/QP: | [Resources]: Sharron Sylvester (OreWin Pty Ltd.) | |
| ABSTRACT: | The Gediktepe project is located within the Afyon tectonic zone, which is one of the main tectonic domains in Turkey. The Afyon zone is a belt consisting of generally low-grade weathered metamorphic rocks. It is located between Menderes Massive to the west and the city of Denizli to the south. The Gediktepe regional geology comprises Upper Paleozoic metamorphics and Lower to Middle Miocene intrusives and volcanics. The metamorphics are generally composed of gneiss, schist, mica schist, chlorite schist, phyllite, amphibolite, marble, and quartzite, with varying degrees of metamorphism. These metamorphics are stratigraphically overlain by Triassic carbonates and fragmental units, Jurassic limestone, and upper Cretaceous ophiolitic mélange. Magmatic rock intrusions developed later between the Oligocene and Lower Miocene, due to extensional features in western Anatolia. Those intrusions cut the Paleozoic metamorphic and Upper Cretaceous ophiolitic rocks, establishing in the region what is now called the Alaçam Mountains granites, which outcrop in an arc-shaped geometry over an area of nearly 30 km2. | |
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