Duration of the Ma'adim Vallis/Gusev Crater Hydrogeologic System, Mars

Details Duration of the Ma'adim Vallis/Gusev Crater Hydrogeologic System, Mars Duration of the Ma'adim Vallis/Gusev Crater Hydrogeologic System, Mars

May 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998icar..133...98c&link_type=abstract

Icarus, Volume 133, Issue 1, pp. 98-108.

Mathematics

Logic

44

Scientific paper

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.

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