Dichotomy Boundary at Aeolis Mensae, Mars: Fretted Terrain Developed in a Sedimentary Deposit

Details Dichotomy Boundary at Aeolis Mensae, Mars: Fretted Terrain Developed in a Sedimentary Deposit Dichotomy Boundary at Aeolis Mensae, Mars: Fretted Terrain Developed in a Sedimentary Deposit

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1824i&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1824

Physics

Scientific paper

Fretted terrain in Aeolis Mensae, Mars, developed in a sedimentary
deposit. A thick, massive unit with a capping layer or duricrust
overlies a more durable layered sequence. Wind, collapse, and minor
fluvial activity contributed to degradation.

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