The differences between the surface geology of Mars and earth are discussed. Sedimentary processes and fluvial systems on Mars are examined. Surface mapping reveals the more recent depostional patterns. In future missions, radar sounding, active seismic systems, and on site deep drilling may be required to fully document the depositional history. For the present, identification of sedimentary layers must rest on localities of tectonic or erosional windows, detection of buried surfaces by indirect methods, and deposition or off lap patterns of distribution.
The Martian sedimentary record
1987-01-01
Aufsatz (Konferenz)
Keine Angabe
Englisch
Martian sediments and sedimentary rocks
NTRS | 1988
|Record-breaking Martian Odyssey
Online Contents | 2011
|NTRS | 1991
|NTRS | 1987
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