Tantalo–Niobate from the Apollo-17 Regolith
- Авторы: Mokhov A.V.1, Kartashov P.M.1, Rybchuk A.P.1, Gornostaeva T.A.1, Bogatikov O.A.1
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Учреждения:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Выпуск: Том 478, № 1 (2018)
- Страницы: 112-114
- Раздел: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/192045
- DOI: https://doi.org/10.1134/S1028334X18010245
- ID: 192045
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Аннотация
Particles of tantalo–niobate of the ferrotantalite-manganotantalite series are discovered for the first time in two lunar regolith fragments delivered by the Apollo-17 mission. Allochtonous and autochtonous mineralization that accompanies tantalo–niobate in the regolith is described. An attempt is made to explain the formation of tantalite in anorthosites of the continental region of the Moon.
Об авторах
A. Mokhov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Автор, ответственный за переписку.
Email: avm8okhov@gmail.com
Россия, Moscow, 119017
P. Kartashov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Россия, Moscow, 119017
A. Rybchuk
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Россия, Moscow, 119017
T. Gornostaeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Россия, Moscow, 119017
O. Bogatikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Россия, Moscow, 119017
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