On the possibility of clathrate hydrates on the Moon

被引：13

作者：

Duxbury, NS

Nealson, KH

Romanovsky, VE

机构：

[1] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA

[2] Univ Alaska, Inst Geophys, Fairbanks, AK 99701 USA

来源：

JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS | 2001年 / 106卷 / E11期

关键词：

D O I：

10.1029/2000JE001425

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

One of the most important inferences of the Lunar Prospector mission data was the existence of subsurface water ice in the permanently shadowed craters near both lunar poles [Feldman et al., 1998]. We propose and substantiate an alternative explanation that hydrogen can exist in the shallow lunar subsurface in the form of clathrate hydrates: CH4 . 6H(2)O and/or CO2 . 6H(2)O.

引用

页码：27811 / 27813

页数：3

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