FAULT-RELATED METAMORPHISM AND ASSOCIATED GOLD MINERALIZATION FOLD SYSTEMS, AS ILLUSTRATED BY THE SOUTHERN URALS

dc.contributor.author	Rudskiy V.G.
dc.date.accessioned	2020-11-02T00:32:32Z
dc.date.available	2020-11-02T00:32:32Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31156372
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 5, 123-125
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18383
dc.description.abstract	Fault-related metamorphism is one of the types of dynamic metamorphism whose allochemical crystalloblastic processes develop in deep fault zones under considerable dynamic load and involve gas-liquid fluids. The proposed model of fault-related metamorphism is the result of work done by us in the Kumak gold deposit in the central ore-bearing part of the Kumak-Kotansinskaya warped zone, a fragment of the regional geosuture called the Chelyabinsk-Taldyk deep fault. This ore deposit, whose geologic structure was analyzed by us earlier, is in the narrowest part of the meridionally extending Anikhovskiy graben-synclinorium that separates the Adamovskiy and the Tekel'dytau horst-anticlinoria, or polymetamorphic complexes (PMC).
dc.title	FAULT-RELATED METAMORPHISM AND ASSOCIATED GOLD MINERALIZATION FOLD SYSTEMS, AS ILLUSTRATED BY THE SOUTHERN URALS
dc.type	Статья

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