GEOCHEMISTRY AND PROTOLITH NATURE OF METABASITES FROM THE TEREKTY BLUESCHIST-GREENSCHIST COMPLEX (GORNY ALTAI)

dc.contributor.author	Volkova N.I.
dc.date.accessioned	2022-01-13T08:02:20Z
dc.date.available	2022-01-13T08:02:20Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13430907
dc.identifier.citation	Doklady Earth Sciences, 2003, 393, 8, 1170-1173
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34259
dc.description.abstract	In the sampled section by Nizhnyaya Katanda river the Uimon series is represented by a package of tectonic plates composed primarily from metabasites, metagraywackes, quartzites with piedmontite and spessartite, shallow marble lentils. The differences in rock chemical composition are established between galucophane and green schist within one section, which determine the observed composition variations of Uimon series' metabasite amphiboles. Metapelites reconstructed as graywackes can be considered as volcagenic-sedimentary phases of underwater volcano' flank zones, and stratified metastreaks and marble - as ancient pelagic sediments and shoal-marina carbonate rocks of seamount sedimentary mantle respectively.
dc.title	GEOCHEMISTRY AND PROTOLITH NATURE OF METABASITES FROM THE TEREKTY BLUESCHIST-GREENSCHIST COMPLEX (GORNY ALTAI)
dc.type	Статья

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