Инд. авторы: Khromykh S.V., Kotler P.D., Smirnov S.Z., Travin A.V., Vladimirov A.G., Sokolova E.N., Oitseva T.A., D'yachkov B.A., Kuzmina O.N., Mizernaya M.A., Agaliyeva B.B.
Заглавие: Rare-metal pegmatite deposits of the kalba region, eastern kazakhstan: age, composition and petrogenetic implications
Библ. ссылка: Khromykh S.V., Kotler P.D., Smirnov S.Z., Travin A.V., Vladimirov A.G., Sokolova E.N., Oitseva T.A., D'yachkov B.A., Kuzmina O.N., Mizernaya M.A., Agaliyeva B.B. Rare-metal pegmatite deposits of the kalba region, eastern kazakhstan: age, composition and petrogenetic implications // Minerals. - 2020. - Vol.10. - Iss. 11. - P.1-15. - EISSN 2075-163X.
Внешние системы: DOI: 10.3390/min10111017; РИНЦ: 45138498; WoS: 000593353600001;
Реферат: eng: The paper presents new geological, mineralogical, and isotope geochronological data for rare-metal pegmatites in the Kalba granitic batholith (Eastern Kazakhstan). Mineralization is especially abundant in the Central-Kalba ore district, where pegmatite bodies occur at the top of large granite plutons and at intersections of deep faults. The pegmatites contain several successive mineral assemblages from barren quartz-microcline and quartz-microcline-albite to Li-Cs-Ta-Nb-Be-Sn-bearing cleavelandite-lepidolite-spodumene. Ar-Ar muscovite and lepidolite ages bracket the metallogenic event between 291 and 286 Ma. The pegmatite mineral deposits formed synchronously with the emplacement of the phase 1 Kalba granites during the evolution of hydrous silicate rare-metal magmas that are produced by the differentiation of granite magma at large sources with possible inputs of F and rare metals with fluids.
Ключевые слова: Rare-Metal Pegmatites; Ar-Ar isotope age; Kalba granite batholith; Eastern Kazakhstan;
Издано: 2020
Физ. характеристика: с.1-15
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