Relaxation of the Martian Crustal Dichotomy Boundary in the Ismenius Region

Details Relaxation of the Martian Crustal Dichotomy Boundary in the Ismenius Region Relaxation of the Martian Crustal Dichotomy Boundary in the Ismenius Region

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1362g&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1362

Mathematics

Logic

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Scientific paper

We present an elasto-visco-plastic finite-element model for the
relaxation of the Martian dichotomy boundary. Our approach is to model
the detailed geologic history of the Ismenius region of Mars, including
slope, strain, and timing of faulting.

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