ТУРМАЛИН-СОДЕРЖАЩИЕ МЕТАСОМАТИТЫ УРАЛЬСКИХ ИЗУМРУДНЫХ КОПЕЙ. СТАТЬЯ II. СЛЮДИТЫ (ФЛОГОПИТЫ)

dc.contributor.author	Бакшеев И.А.
dc.contributor.author	Кудрявцева О.Е.
dc.contributor.author	Беляцкий Б.В.
dc.contributor.author	Попов М.П.
dc.contributor.author	Саранцева Н.П.
dc.contributor.author	Выдрин М.В.
dc.date.accessioned	2022-02-25T04:02:35Z
dc.date.available	2022-02-25T04:02:35Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=9509641
dc.identifier.citation	Уральский геологический журнал, 2003, , 4(34), 3-34
dc.identifier.issn	2219-1208
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/35739
dc.description.abstract	Tourmalines from phlogopitite, pockets, and cut veinlets can be classified as variety between the shorl-dravite endmembers with the Feобщ.*100%/(Fe общ.+Mg) ratio ranging from 16.4 to 30.3%. Based on the F- contents tourmaline composition ranges from hydroxy- to fluor-dravite. Temperature of tourmaline crystallization estimated from the tourmaline-biotite thermometer is 360-490°C. Phlogopitite, pockets, and cut veinlets have been formed at the fF2 increasing and low values of fO2 and fCO2. Absolute age of phlogopitite estimated from Rb/Sr and Sm/Nd methods is about 210 Ma.
dc.title	ТУРМАЛИН-СОДЕРЖАЩИЕ МЕТАСОМАТИТЫ УРАЛЬСКИХ ИЗУМРУДНЫХ КОПЕЙ. СТАТЬЯ II. СЛЮДИТЫ (ФЛОГОПИТЫ)
dc.type	Статья
dc.subject.udc	549.6+549.612(234.852)

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