Geochemical Evolution and Ore-Bearing Metasomatic Rocks of the Baga-Gazryn Multiphase Massif of Rare-Metal Li–F Granites (Mongolia)
- Авторлар: Antipin V.S.1, Kuzmin M.I.1, Odgerel D.2, Kousch L.V.1, Perepelov A.B.1
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Мекемелер:
- Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences
- Institute of Paleontology and Geology, Mongolian Academy of Sciences
- Шығарылым: Том 483, № 1 (2018)
- Беттер: 1468-1472
- Бөлім: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/194363
- DOI: https://doi.org/10.1134/S1028334X18110168
- ID: 194363
Дәйексөз келтіру
Аннотация
This paper considers the geochemical evolution of igneous and metasomatic rocks in the Baga-Gazryn Massif on the basis of new precision analytical data. The Baga-Gazryn rocks are characterized by enrichment in F, which is concentrated in Li–F mica, topaz, and fluorite. Along with F, zwitters and microclinites are enriched in Li, Rb, Cs, and ore elements Sn, W, Zn. High-charge elements (Zr, Hf, Nb, Ta, and Ti) and also Th and U are not very different in the Baga-Gazryn granites of various phases and metasomatic rocks.
Авторлар туралы
V. Antipin
Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences
Хат алмасуға жауапты Автор.
Email: antipin@igc.irk.ru
Ресей, Irkutsk, 664033
M. Kuzmin
Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences
Email: antipin@igc.irk.ru
Ресей, Irkutsk, 664033
D. Odgerel
Institute of Paleontology and Geology, Mongolian Academy of Sciences
Email: antipin@igc.irk.ru
Моңғолия, Ulan-Bator, 210351
L. Kousch
Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences
Email: antipin@igc.irk.ru
Ресей, Irkutsk, 664033
A. Perepelov
Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences
Email: antipin@igc.irk.ru
Ресей, Irkutsk, 664033
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