Modeling Martian Thermokarst Subsidence with Magmatic Melting of Permafrost

Details Modeling Martian Thermokarst Subsidence with Magmatic Melting of Permafrost Modeling Martian Thermokarst Subsidence with Magmatic Melting of Permafrost

Mar 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpi....38.2422m&link_type=abstract

38th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXVIII), held March 12-16, 2007 in League City, Texas

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Scientific paper

Computational time dependent models of martian permafrost melting by
magma chamber intrusion produce topographic moats around volcanoes in
regions where thermal gradients, surface temperatures, or porosities are
higher than average.

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