PHYSICAL CHARACTERISTICS OF MEGACRYSTAL HIGH PRESSURE PHASES

dc.contributor.author	Milyutin S.A.
dc.contributor.author	Genshaft Y.S.
dc.contributor.author	Saltykovski A.Y.
dc.contributor.author	Kuznetsova L.G.
dc.contributor.author	Lukert U.
dc.contributor.author	Budzinski G.
dc.contributor.author	Reiche M.
dc.date.accessioned	2020-11-07T08:52:21Z
dc.date.available	2020-11-07T08:52:21Z
dc.date.issued	1992
dc.identifier	https://elibrary.ru/item.asp?id=31111026
dc.identifier.citation	Journal of Geodynamics, 1992, , 3, 169-184
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18683
dc.description.abstract	The composition and structural features of megacrystals of garnets, ilmenites, monoclinic pyroxenes, K-Na-feldspars occurring as inclusions in the Cenozoic alkaline basalts of Mongolia have been studied by means of X-ray diffractometry, i.r.-spectroscopy and electrone microscopy. The density of megacrystals has been determined by means of hydrostatic weighing. The high-temperature and deep formation of megacrystals are discussed.
dc.subject	Cenozoic	en
dc.title	PHYSICAL CHARACTERISTICS OF MEGACRYSTAL HIGH PRESSURE PHASES
dc.type	Статья
dc.subject.age	Кайнозой	ru
dc.subject.age	Cenozoic	en

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