Duration of the Ma'adim Vallis/Gusev crater hydrogeologic system, Mars

被引：65
|
作者：
Cabrol, NA
Grin, EA
Landheim, R
Kuzmin, RO
Greeley, R
机构：
[1] NASA, Ames Res Ctr, Ctr Mars Explorat, Div Space Sci, Moffett Field, CA 94035 USA
[2] NASA, Ames Res Ctr, SETI Inst, Ctr Mars Explorat, Moffett Field, CA 94035 USA
[3] Russian Acad Sci, Vernadsky Inst, Moscow 117975, Russia
[4] Arizona State Univ, Dept Geol, Tempe, AZ 85287 USA
来源：
ICARUS | 1998年 / 133卷 / 01期
关键词：
Mars; surface; geological processes; planets;
D O I：
10.1006/icar.1998.5914
中图分类号：
P1 [天文学];
学科分类号：
0704 ;
摘要：
Ma'adim Vallis and Gusev crater (Aeolis subquadrangle of Mars) formed a complex hydrogeologic system through time. Crater statistics over five geologic units, coupled with morphologic and geologic observations, show that this system was active over a period ranging from 0.7 to about 2 billion years. These results make the floor of Gusev crater one of the most prominent martian depositional features. The last aqueous sedimentary deposition could have occurred during Early Amazonian. (C) 1998 Academic Press.
引用
收藏
页码：98 / 108
页数：11
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