Flexural Response to Sediment Erosion and Unloading at Valles Marineris, Mars

Details Flexural Response to Sediment Erosion and Unloading at Valles Marineris, Mars Flexural Response to Sediment Erosion and Unloading at Valles Marineris, Mars

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2557d&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2557

Physics

1

Scientific paper

Models of the Valles Marineris formation have difficulty accounting for
the observed gravity and topography surrounding the troughs. We show
that these features can be explained by lithospheric flexure in response
to the erosion of ancient sediments.

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