Инд. авторы:	Pilitsyna A.V., Tretyakov A.A., Alifirova T.A., Degtyarev K.E., Kovalchuk E.V.
Заглавие:	The first find of spinel peridotite in the Southern Kazakhstan: Structure, composition, and parameters of high-pressure metamorphism
Библ. ссылка:	Pilitsyna A.V., Tretyakov A.A., Alifirova T.A., Degtyarev K.E., Kovalchuk E.V. The first find of spinel peridotite in the Southern Kazakhstan: Structure, composition, and parameters of high-pressure metamorphism // Doklady Earth Sciences. - 2017. - Vol.476. - Iss. 1. - P.982-985. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы:	DOI: 10.1134/S1028334X17090069; SCOPUS: 2-s2.0-85030686262; WoS: 000412358700003;
Реферат:	eng: Spinel peridotite, metamorphosed in high-pressure conditions, was first described within the Western part of the Central Asian Orogenic Belt. The spinel peridotite has the characteristics of Mg–Cr ultramafites indicating the mantle origin of its protolith. The preliminary estimation of the metamorphism peak for the model system MgO–Al2O3—SiO2–Cr2O3 (MASCr) is 10–19 kbar at 680–800°C. © 2017, Pleiades Publishing, Ltd.
Ключевые слова:	High-pressure condition; Kazakhstan; Model system; Spinel peridotites; Earth sciences; high pressure; metamorphism; orogenic belt; peridotite; spinel; Kazakhstan; Protoliths; Central Asian orogenic belt; High pressure metamorphism;
Издано:	2017
Физ. характеристика:	с.982-985