CHLORITIC ROCKS AND CHLORITIZED BASALTS AS PLAUSIBLE PRECURSORS OF METAMORPHIC PERIDOTITES AND PYROXENITES IN THE KOKCHETAV MASSIF, NORTHERN KAZAKHSTAN

dc.contributor.author	Reverdatto V.V.
dc.contributor.author	Selyatitskiǐ A.Yu.
dc.date.accessioned	2022-08-14T03:31:11Z
dc.date.available	2022-08-14T03:31:11Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13472511
dc.identifier.citation	Doklady Earth Sciences, 2004, 394, 1, 130-133
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38546
dc.description.abstract	Inordinary and similar chemical composition of garnet peridotites and spinel harzburgites allows suggesting that they were formed from chlorite rocks contained in the upper part of Earth crust. Submerging to the depth of 100-150 km upon subduction has lead to metamorphism of these rocks. Associating with harzburgites pyroxenites were formed on the base of chloritized basalts, as concluded from geological and geochemical data analysis.
dc.title	CHLORITIC ROCKS AND CHLORITIZED BASALTS AS PLAUSIBLE PRECURSORS OF METAMORPHIC PERIDOTITES AND PYROXENITES IN THE KOKCHETAV MASSIF, NORTHERN KAZAKHSTAN
dc.type	Статья

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