Physics
Scientific paper
Mar 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1993w&link_type=abstract
33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1993
Physics
Scientific paper
Normal fault scarps at Tempe Terra have much lower slopes (<30°)
than expected for faults forming in an Andersonian stress regime. We
discuss three possible mechanisms responsible for forming fault scarp
slopes <30°: low coefficients of friction, fault rotation, and
scarp degradation.
Schultz Richard A.
Wilkins Scott J.
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