Enviar artigo por via de e-mail Tantalo–Niobate from the Apollo-17 Regolith
- Autores: Mokhov A.V.1, Kartashov P.M.1, Rybchuk A.P.1, Gornostaeva T.A.1, Bogatikov O.A.1
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Afiliações:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Edição: Volume 478, Nº 1 (2018)
- Páginas: 112-114
- Seção: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/192045
- DOI: https://doi.org/10.1134/S1028334X18010245
- ID: 192045
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Resumo
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.
Sobre autores
A. Mokhov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Autor responsável pela correspondência
Email: avm8okhov@gmail.com
Rússia, Moscow, 119017
P. Kartashov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Rússia, Moscow, 119017
A. Rybchuk
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Rússia, Moscow, 119017
T. Gornostaeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Rússia, Moscow, 119017
O. Bogatikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Rússia, Moscow, 119017
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