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


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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.

作者简介

P. Kartashov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: avm8okhov@gmail.com
俄罗斯联邦, Moscow, 109017

A. Mokhov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

编辑信件的主要联系方式.
Email: avm8okhov@gmail.com
俄罗斯联邦, Moscow, 109017

T. Gornostaeva

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: avm8okhov@gmail.com
俄罗斯联邦, Moscow, 109017

O. Bogatikov

Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry

Email: avm8okhov@gmail.com
俄罗斯联邦, Moscow, 109017

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