GENESIS OF THE NYURUNDUKAN ULTRAMAFIC-MAFIC PLUTON, BAIKAL MOUNTAIN LAND

dc.contributor.author	Tsygankov A.A.
dc.contributor.author	Filimonov A.V.
dc.contributor.author	Vrublevskaya T.T.
dc.contributor.author	Travkin A.V.
dc.date.accessioned	2021-06-07T12:43:27Z
dc.date.available	2021-06-07T12:43:27Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=13393920
dc.identifier.citation	Petrology, 2002, 10, 1, 52-77
dc.identifier.issn	0869-5911
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/28875
dc.description.abstract	Genesis of the Nyurundukan ultramafic-Mafic pluton, Baikal mountain land was discussed. The massif was determined to consist of three intrusive phases, each of which was accompanied dike rocks. The results demonstrated that a melt of phase-II gabbroids composition can be produced by the fractional crystallization of picobasalt that was parental for the first intrusive phase in an intermediate chamber at a pressure of 12 kbar.
dc.title	GENESIS OF THE NYURUNDUKAN ULTRAMAFIC-MAFIC PLUTON, BAIKAL MOUNTAIN LAND
dc.type	Статья

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