Sequential faulting history of Valles Marineris, Mars

Details Sequential faulting history of Valles Marineris, Mars Sequential faulting history of Valles Marineris, Mars

Mar 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997lpi....28..371f&link_type=abstract

Conference Paper, 28th Annual Lunar and Planetary Science Conference, p. 371.

Mathematics

Logic

Mars Surface, Geological Faults, Valleys, Tectonics, Planetary Geology, Plateaus, Planetary Evolution

Scientific paper

The location and orientation of the shallow faults that characterize the plateau in the Valles Marineris region of Mars are investigated to derive the sequential extensional tectonic history of the region. The stress trajectories developed for the Valley suggest that two episodes (northwesterly and northeasterly) of faulting occurred prior to the greatest extensional direction (north-south) that most likely created the Valley proper and surrounding parallel grabens. These results independently confirm the relatively young formation of the Valley.

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