Elastic Thickness, Paleo Heat Flow, and Curie Depth at the Tyrrhena Patera Highland Volcano

Details Elastic Thickness, Paleo Heat Flow, and Curie Depth at the Tyrrhena Patera Highland Volcano Elastic Thickness, Paleo Heat Flow, and Curie Depth at the Tyrrhena Patera Highland Volcano

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1750g&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1750

Computer Science

Scientific paper

Admittance modeling of the Tyrrhena Patera highland volcano indicates
substantial surface heat flows between 26 and 82 mW/m^2 at the time of
load emplacement, compatible with Curie depths of 9-29,
15-48 and 17-56 km for pyrrhotite, magnetite, and hematite,
respectively.

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