A description of surface features in north Tyrrhena Terra, Mars: Evidence for extension and lava flooding

Details A description of surface features in north Tyrrhena Terra, Mars: Evidence for extension and lava flooding A description of surface features in north Tyrrhena Terra, Mars: Evidence for extension and lava flooding

Nov 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007icar..191..524c&link_type=abstract

Icarus, Volume 191, Issue 2, p. 524-544.

Mathematics

Logic

4

Scientific paper

We studied north Tyrrhena Terra, an approximately 39,000 km2 area, located in the transition region straddling the Amenthes and Mare Tyrrhenum Mars Chart quadrangles 14 and 22, respectively. The study area comprises ancient terrains with infilled craters, ridges and valleys. Interpretation of orbiter data of ancient terrains is inherently difficult, but valuable information can be obtained using multiple datasets and analyzing various geological features. Using data from the High Resolution Stereo Camera on board Mars Express, complemented by Mars Global Surveyor MOLA DEM and MOC Narrow Angle datasets, we observed and interpreted surface morphologies at a scale suitable for geologic investigation. Morphometric examination of a 31 km diameter large impact crater indicated that tectonism and volcanism were responsible for its morphologic modification. Small impact crater depth/diameter relationships indicated that smooth surfaces of valleys are composed of highly consolidated material. Surface cracks and lobate fronts further suggested that the rocks are volcanic. Examination of tectonic features revealed that in the study area: a dominant NW SE fabric is related to a ridge/bench scarp valley repetition consistent with synthetic and antithetic normal faulting; a NNW SSE lineament represents the surface expression of normal faulting post-dating all other tectonic features. A weak NE SW fabric is observable as small sublinear depressions, and at the contact between units internal to one large crater. One 20 km diameter crater in the study area was interpreted to be a caldera, infilled by thick volcanic rock layers. Identification of wrinkle ridges further indicated that thick layered lava flows infilled the main depressions of the study area. The available evidence suggests that the study area underwent multiple episodes of extension and volcanism.

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