HALOGENS IN MICAS OF VOLCANIC ROCKS OF THE KURILE-KAMACHATKA ISLAND-ARC SYSTEM

dc.contributor.author	Volynets O.N.
dc.contributor.author	Bushyakov I.N.
dc.contributor.author	Voronina L.K.
dc.date.accessioned	2020-10-08T10:27:29Z
dc.date.available	2020-10-08T10:27:29Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31094135
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 6, 189-192
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17795
dc.description.abstract	The role of volatiles in island-arc magma generation is widely discussed in the geologic literature. Two of the most important volatile mineralizers are fluorine and chlorine, whose principal accumulator minerals in igneous rocks include mica. The authors used the X-ray spectroscopic method to study the distribution of these elements in micas from 83 samples of volcanic rocks of the Kurile-Kamchatka island-arc system.
dc.title	HALOGENS IN MICAS OF VOLCANIC ROCKS OF THE KURILE-KAMACHATKA ISLAND-ARC SYSTEM
dc.type	Статья

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