Signs of Hydrothermal Activity in Lunar Rocks according to the Data of a Regolith Investigation
- Авторы: Kartashov P.M.1, Mokhov A.V.1, Gornostaeva T.A.1, Bogatikov O.A.1
-
Учреждения:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
- Выпуск: Том 480, № 2 (2018)
- Страницы: 810-813
- Раздел: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/193452
- DOI: https://doi.org/10.1134/S1028334X18060260
- ID: 193452
Цитировать
Аннотация
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.
Об авторах
P. Kartashov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Россия, Moscow, 109017
A. Mokhov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Автор, ответственный за переписку.
Email: avm8okhov@gmail.com
Россия, Moscow, 109017
T. Gornostaeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Россия, Moscow, 109017
O. Bogatikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry
Email: avm8okhov@gmail.com
Россия, Moscow, 109017
Дополнительные файлы
