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Okrostsvaridze, Avtandil and Bluashvili, David (2009) The Sakeni Ore Field (Greater Caucasus) – Geological Evidence and Prospects. Bulletin of the Georgian National Academy of Sciences. ISSN 0132 - 1447
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Abstract
In the crystalline basement of the Greater Caucasus, in the contact zone between the Upper Variscan Sakeni intrusive of dioritic-granodioritic composition of the mantle-crust generation and the PreAlpine anatectic granite-migmatitic complex, the authors have discovered the Sakeni ore field. Here, four isolated ore-manifestations of quartz-gold-low sulfide hydrothermal genetic type have been established, formed at a medium depth (2-3km), that are entirely controlled by the Alibek regional overthrust and a system of young cross faults. Recent erosion strips mainly the frontal part of low temperature quartz-gold-antimonite mineralization. Due to it, in the deeper horizons, more important gold stockwork type mineralization is expected.
| Item Type: | Article |
|---|---|
| Subjects: | Q Science > QE Geology |
| Depositing User: | ავთანდილ ოქროსცვარიძე |
| Date Deposited: | 24 Mar 2022 07:11 |
| Last Modified: | 24 Mar 2022 07:11 |
| URI: | http://eprints.iliauni.edu.ge/id/eprint/11013 |
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