Signs of Hydrothermal Activity in Lunar Rocks according to the Data of a Regolith Investigation


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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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