DISTRIBUTION OF LOBATE DEBRIS APRONS AND SIMILAR FLOWS ON MARS

被引:183
作者
SQUYRES, SW [1 ]
机构
[1] CORNELL UNIV, PLANETARY STUDIES LAB, ITHACA, NY 14853 USA
来源
JOURNAL OF GEOPHYSICAL RESEARCH | 1979年 / 84卷
关键词
D O I
10.1029/JB084iB14p08087
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
Planet-wide mapping of lobate debris aprons and other similar flows on Mars shows a strong concentration in two latitudinal bands roughly 25o wide and centered at 40oN and 45oS. This distribution supports the idea that these flows form when eorsional debris is transported downslope and becomes mixed with ice deposited from the atmosphere, as these latitudes should receive high seasonal H2O frost deposition relative to the rest of the planet. -from Author Dept. of Geological Sciences and Laboratory for Planetary Studies, Cornell University, Ithaca, New York 14853, U.S.A.
引用
收藏
页码:8087 / 8096
页数:10
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