Age, Composition, and Geodynamic Environments for the Formation of Granites and Lithium-rich Rare-Element Pegmatite of Khusuingol Field (Sangilen Highlands)
- Авторлар: Sergeev S.A.1, Kuznetsova L.G.2, Shokalsky S.P.1
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Мекемелер:
- Karpinskii Russian Geological Institute (VSEGEI)
- Vinogradov Institute of Geochemistry, Siberian Branch
- Шығарылым: Том 482, № 2 (2018)
- Беттер: 1311-1316
- Бөлім: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/194200
- DOI: https://doi.org/10.1134/S1028334X18100070
- ID: 194200
Дәйексөз келтіру
Аннотация
The composition, age, and genetic relationships of spodumene pegmatites of the Khusuingol field (South Sangilen pegmatite belt, SW Sayan), encompassing the large Tastyg lithium deposit, with granitoids of the neighboring polygenic Dzos-Khusuingol batholith have been studied. SHRIMP-II U–Pb zircon analyses yielded an Early Paleozoic age of the granites and pegmatites. The tectonic settings of the formation of these rocks are discussed.
Авторлар туралы
S. Sergeev
Karpinskii Russian Geological Institute (VSEGEI)
Email: lkuzn@igc.irk.ru
Ресей, St. Petersburg
L. Kuznetsova
Vinogradov Institute of Geochemistry, Siberian Branch
Хат алмасуға жауапты Автор.
Email: lkuzn@igc.irk.ru
Ресей, Irkutsk
S. Shokalsky
Karpinskii Russian Geological Institute (VSEGEI)
Email: lkuzn@igc.irk.ru
Ресей, St. Petersburg
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