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

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

doi:10.1134/S1028334X18060260

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

作者: Kartashov P.M.¹, Mokhov A.V.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 480, 编号 2 (2018)
页面: 810-813
栏目: Geochemistry
URL: https://ogarev-online.ru/1028-334X/article/view/193452
DOI: https://doi.org/10.1134/S1028334X18060260
ID: 193452

如何引用文章

全文:

开放存取

##reader.subscriptionAccessGranted##
受限制的访问

订阅存取

详细
作者简介
参考
补充文件
统计

详细

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.