Stress Differences in the Martian Interior: Constraints on the Thermal State of Mars

Details Stress Differences in the Martian Interior: Constraints on the Thermal State of Mars Stress Differences in the Martian Interior: Constraints on the Thermal State of Mars

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1567a&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1567

Physics

Scientific paper

Using the elastic thick shell model the stress differences determined in
the martian mantle are about 100 MPa at a 100 depth and about 60-70 MPa
in the upper 300 km. To sustain these stresses a temperature of 730C is
required at 100 km depth and about 800C at 300 depth.

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