New type of gold mineralization of the Tyrnyauz ore cluster (Kabardino-Balkar Republic)


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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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