Email this article New type of gold mineralization of the Tyrnyauz ore cluster (Kabardino-Balkar Republic)
- Authors: Parada S.G.1, Popov Y.V.2, Stolyarov V.V.1
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Affiliations:
- Institute of Arid Zones, Southern Science Center
- Southern Federal University
- Issue: Vol 477, No 1 (2017)
- Pages: 1256-1259
- Section: Geology
- URL: https://bakhtiniada.ru/1028-334X/article/view/191322
- DOI: https://doi.org/10.1134/S1028334X17110058
- ID: 191322
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Abstract
Native Au on the northern flank of the Tyrnyauz ore cluster is related to the pyroxene–garnet association of skarns and is represented by separate idiomorphic ingrowths in rock-forming minerals of skarns and relatively isometric xenomorphic grains in the interstices. Gold mineralization can be attributed to the Au-skarn geological–industrial type with ores of a low-sulfide formation and Au–Bi–Te geochemical specialization.
About the authors
S. G. Parada
Institute of Arid Zones, Southern Science Center
Author for correspondence.
Email: parada@ssc-ras.ru
Russian Federation, Rostov-on-Don, 344006
Yu. V. Popov
Southern Federal University
Email: parada@ssc-ras.ru
Russian Federation, Rostov-on-Don, 344090
V. V. Stolyarov
Institute of Arid Zones, Southern Science Center
Email: parada@ssc-ras.ru
Russian Federation, Rostov-on-Don, 344006
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