Sedimentary Facies, Subaqueous Sediment Transport, and Depositional Environment of the Burns Formation, Meridiani Planum

Details Sedimentary Facies, Subaqueous Sediment Transport, and Depositional Environment of the Burns Formation, Meridiani Planum Sedimentary Facies, Subaqueous Sediment Transport, and Depositional Environment of the Burns Formation, Meridiani Planum

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2254g&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2254

Physics

1

Scientific paper

The bedrock stratigraphy at the Opportunity Landing Site defines a
"wetting-upward" succession which records a progressive increase in the
influence of groundwater and, ultimately, surface water in controlling
primary depositional processes.

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