HYPERSTHENE HORNFELSES OF THE KANDYGATAI COMPLEX, EASTERN KAZAKHSTAN

dc.contributor.author	Sukhorukov V.P.
dc.contributor.author	Plotnikov A.V.
dc.date.accessioned	2022-07-25T04:36:24Z
dc.date.available	2022-07-25T04:36:24Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13461971
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 973-977
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38386
dc.description.abstract	The Kandygatai metamorphic block is situated within the Zharma strike-slip zone, which separates the Hercynides of the Zaisan and Caledonides of the Chingiz-Tarbagatai fold systems. Metapelites of the Kandygatai Complex have already been considered in the literature. Based on findings of hypersthenesillimanite, corundum-garnet, and hypersthene-clinopyroxene assemblages, this complex was attributed to the high-pressure granulites (T = 950-1000°C, P = 10-12 kbar and interpreted as an ancient sialic basement unique for this region. The present paper considers new petrological data, which make it possible to attribute this complex to the high-temperature-lowpressure rocks and propose a two-stage model of its formation.
dc.title	HYPERSTHENE HORNFELSES OF THE KANDYGATAI COMPLEX, EASTERN KAZAKHSTAN
dc.type	Статья

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