GLIMMERITES AND SIMILAR ROCKS IN MIDDLE ASIA

dc.contributor.author	Khamrabayev I.K.
dc.contributor.author	Iskandarov E.
dc.contributor.author	Khamrabayeva Z.I.
dc.contributor.author	Nasyrova G.I.
dc.date.accessioned	2020-11-09T07:48:58Z
dc.date.available	2020-11-09T07:48:58Z
dc.date.issued	1992
dc.identifier	https://elibrary.ru/item.asp?id=38602319
dc.identifier.citation	Известия Российской академии наук. Серия геологическая, 1992, , 5, 52-61
dc.identifier.issn	0321-1703
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18762
dc.description.abstract	New petrographic descriptions and analyses of the mica of glimmerite (or slyudite) and similar rocks found in xenoliths from explosion pipes, dikes and intrusives of the Central and South Tien Shan and East Pamirs are given. It is concluded that glimmerite generally forms metasomatically, from various rocks and at various depths in the lithosphere, including the upper crust. Corrections should be made in current petrographic handbooks, in which glimmerite is defined as an igneous rock.
dc.title	GLIMMERITES AND SIMILAR ROCKS IN MIDDLE ASIA
dc.type	Статья

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