Fluid inclusions in minerals and zonation of scapolite metasoms (Eastern Pamir).

dc.contributor.author	Rysaeva I.
dc.contributor.author	Rafikova F.
dc.contributor.author	Kubishkina E.
dc.date.accessioned	2018-09-19T22:50:15Z
dc.date.available	2018-09-19T22:50:15Z
dc.date.issued	2016
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/145604
dc.description.abstract	In the article the questions of Geochemistry and Mineralogy scapolite Deposit of the East Pamirs. Scapolite mineralization is localized in metasomatity Alpine veins. Scapolite occurs in three generations. Early metamorphic scapolite. Milky-white coarse-grained scapolite. Jewelry clear crystals of scapolite from a later generation. Scapolite different generations differ on a number of indicators. The temperature and pressure of mineral formation, the concentration of the solutions and their composition scapolite different.
dc.subject	Fluid inclusions
dc.subject	Generations
dc.subject	Metamorphism
dc.subject	Mineral
dc.subject	Scapolite
dc.subject	Temperature
dc.title	Fluid inclusions in minerals and zonation of scapolite metasoms (Eastern Pamir).
dc.type	Article
dc.relation.ispartofseries-issue	6
dc.relation.ispartofseries-volume	7
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	2944
dc.source.id	SCOPUS-2016-7-6-SID85004072355

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Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.