Temporal Variability in Tharsis Stress State Based on Wrinkle Ridges and Strike-Slip Faulting

Details Temporal Variability in Tharsis Stress State Based on Wrinkle Ridges and Strike-Slip Faulting Temporal Variability in Tharsis Stress State Based on Wrinkle Ridges and Strike-Slip Faulting

Mar 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004lpi....35.1101o&link_type=abstract

35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, abstract no.1101

Computer Science

1

Scientific paper

An observed transition from wrinkle ridge formation to strike-slip
faulting suggests a decrease in circum-Tharsis compressional stress from
~3 4x lithostatic load (rgz) during the Mid Hesperian to ~1.5x rgz by
the start of the Amazonian.

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