Signs of Hydrothermal Activity in Lunar Rocks according to the Data of a Regolith Investigation
- Autores: Kartashov P.M.1, Mokhov A.V.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 480, Nº 2 (2018)
- Páginas: 810-813
- Seção: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/193452
- DOI: https://doi.org/10.1134/S1028334X18060260
- ID: 193452
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Resumo
Two cases of mineral associations from the samples of regolith delivered by AS Luna 20 and AS Luna 24, which indicate possible hydrothermal alteration of primary lunar rocks, are considered. The probability of hydrothermal processes on the Moon means a drastic change in the firm views of the processes of the formation of lunar mineral.
Sobre autores
P. Kartashov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Rússia, Moscow, 109017
A. Mokhov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Autor responsável pela correspondência
Email: avm8okhov@gmail.com
Rússia, Moscow, 109017
T. Gornostaeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Rússia, Moscow, 109017
O. Bogatikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Rússia, Moscow, 109017
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