Tantalo–Niobate from the Apollo-17 Regolith

A. V. Mokhov; P. M. Kartashov; A. P. Rybchuk; T. A. Gornostaeva; O. A. Bogatikov

doi:10.1134/S1028334X18010245

Tantalo–Niobate from the Apollo-17 Regolith

作者: Mokhov A.V.¹, Kartashov P.M.¹, Rybchuk A.P.¹, Gornostaeva T.A.¹, Bogatikov O.A.¹
隶属关系:
1. Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
期: 卷 478, 编号 1 (2018)
页面: 112-114
栏目: Geochemistry
URL: https://ogarev-online.ru/1028-334X/article/view/192045
DOI: https://doi.org/10.1134/S1028334X18010245
ID: 192045

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详细

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.