ТУРМАЛИН-СОДЕРЖАЩИЕ МЕТАСОМАТИТЫ УРАЛЬСКИХ ИЗУМРУДНЫХ КОПЕЙ, СРЕДНИЙ УРАЛ. СТАТЬЯ III. ТУРМАЛИН-МАРГАРИТОВЫЕ ПРОЖИЛКИ С АЛЬБИТОМ, ФЛОГОПИТОМ И ХЛОРИТОМ

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dc.contributor.author Кудрявцева О.Е.
dc.contributor.author Бакшеев И.А.
dc.contributor.author Попов М.П.
dc.contributor.author Устинов В.И.
dc.date.accessioned 2022-11-17T05:31:45Z
dc.date.available 2022-11-17T05:31:45Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=9509725
dc.identifier.citation Уральский геологический журнал, 2004, , 3(39), 51-68
dc.identifier.issn 2219-1208
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/39775
dc.description.abstract Tourmalines from tourmaline-margarite veinlets can be divided into two groups. The first one is relic from phlogopitite with the FeΣ*100%/(FeΣ+Mg), Ca*100%/(Ca+Na) ratios and flour content ranging from 13.8 to 34.6%, from 18.4 to 45.9%, and from 0.11 to 0.44 apfu, respectively. The second group includes newly formed tourmaline that is simulteneous with margarite. This can be classified as variety between the shorl-dravite endmembers with the FeΣ*100%/(FeΣ+Mg) and Ca*100%/(Ca+Na) ratios ranging from 18.7 to 41.1% and from 5.5 to 16.1%. Based on the F- contents tourmaline composition ranges from dravite to fluor-dravite (0.03-0.72 apfu F). Crystallization temperature of the tourmaline estimated from the tourmaline-biotite thermometer is 350-360°C. Tourmaline-margarite veinlets have been formed at the fF2 increasing and low values of fO2 and fCO2.
dc.title ТУРМАЛИН-СОДЕРЖАЩИЕ МЕТАСОМАТИТЫ УРАЛЬСКИХ ИЗУМРУДНЫХ КОПЕЙ, СРЕДНИЙ УРАЛ. СТАТЬЯ III. ТУРМАЛИН-МАРГАРИТОВЫЕ ПРОЖИЛКИ С АЛЬБИТОМ, ФЛОГОПИТОМ И ХЛОРИТОМ
dc.type Статья
dc.subject.udc 549.6+549.612(234.852)


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