STRUCTURAL ZONING OF POLYFACIES METAMORPHIC COMPLEXES IN SOUTHEAST SIBERIA

dc.contributor.author	Vasil'yev Y.P.
dc.contributor.author	Ivanov A.I.
dc.date.accessioned	2020-04-16T07:09:47Z
dc.date.available	2020-04-16T07:09:47Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=31011494
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1987, 296, 5, 98-100
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16876
dc.description.abstract	One of the forms in which the relationship between tectonic deformation and metamorphism is expressed is structural and metamorphic zoning, i.e., the regular variation of structural parageneses and deformation styles of rocks with the parameters of their metamorphism. In this article, the authors give examples of such zoning in metamorphic complexes of three different types: 1) the Slyudyanka granulite complex, 2) the Khamar Daban complex with andalusite- and sillimanite-type zoning, 3) the Patom complex with kyanite- and sillimanite-type zoning.
dc.title	STRUCTURAL ZONING OF POLYFACIES METAMORPHIC COMPLEXES IN SOUTHEAST SIBERIA
dc.type	Статья

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