Tyrrhena Patera, Mars: Evidence for a solidified magma chamber?

Details Tyrrhena Patera, Mars: Evidence for a solidified magma chamber? Tyrrhena Patera, Mars: Evidence for a solidified magma chamber?

Oct 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011epsc.conf..376g&link_type=abstract

EPSC-DPS Joint Meeting 2011, held 2-7 October 2011 in Nantes, France. http://meetings.copernicus.org/epsc-dps2011, p.376

Physics

Scientific paper

The noachian-aged martian highland volcano Tyrrhena Patera is associated with a well pronounced gravity anomaly and admittance modeling suggests that the observed signal can be explained by a high density surface load. Alternatively, a solidified magma chamber could be present at depth, and subsurface loading could correspond to up to 10 % of the surface load.

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