GEOLOGICAL-STRUCTURAL MODEL OF FORMING OF THE GOLD ORE DEPOSIT OF SOTSK

Authors

  • F. G. Shamtsyan JSC "GAZMETALLINVEST", Moscow, Russia
  • S. U. Vardanyan JSC "GAZMETALLINVEST", Moscow, Russia
  • R. A. Harutyunyan Chair of Mineralogy, Petrology and Geochemistry, YSU, Armenia

DOI:

https://doi.org/10.46991/PYSUC.2003.37.1.121

Keywords:

Sotsk deposit , metamorphic and metasomatic processing, gabbro and peridotites, petrophysical parameters, Republic of Armenia

Abstract

The ore-enclosing rocks of the Sotsk deposit are subject to metamorphic and metasomatic processing. The separate ore bodies with depth combine in one (stock). The main parts of mineralization is timed to extreme parts of gabbro and peridotites, which are distinguished by their petrophysical parameters. The character of gold mineralization distribution testifies, that upper part of deposit is most perspective. The stage of intensive mineralization is distinguished, the mineralization fades with depth. The hard foundation, located at the short depth, is broken up by tectonic breaches which were favourable surroundings for penetration of hydrothermal solution.

Downloads

Published

2003-03-03

Issue

Vol. 37 No. 1 (200) (2003)

Section

Geology

License

Copyright (c) 2003 Proceedings of the YSU

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

How to Cite

GEOLOGICAL-STRUCTURAL MODEL OF FORMING OF THE GOLD ORE DEPOSIT OF SOTSK. (2003). Proceedings of the YSU C: Geological and Geographical Sciences, 37(1 (200), 121-126. https://doi.org/10.46991/PYSUC.2003.37.1.121