GLIMMERITES AND SIMILAR ROCKS IN MIDDLE ASIA

dc.contributor.authorKhamrabayev I.K.
dc.contributor.authorIskandarov E.
dc.contributor.authorKhamrabayeva Z.I.
dc.contributor.authorNasyrova G.I.
dc.date.accessioned2020-11-09T07:48:58Z
dc.date.available2020-11-09T07:48:58Z
dc.date.issued1992
dc.description.abstractNew 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.identifierhttps://elibrary.ru/item.asp?id=38602319
dc.identifier.citationИзвестия Российской академии наук. Серия геологическая, 1992, , 5, 52-61
dc.identifier.issn0321-1703
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/18762
dc.titleGLIMMERITES AND SIMILAR ROCKS IN MIDDLE ASIA
dc.typeСтатья

Файлы

Коллекции