Mantle Convection and Magma Production on Present-Day Mars: The Effects of Temperature-dependent Rheology and Water

Details Mantle Convection and Magma Production on Present-Day Mars: The Effects of Temperature-dependent Rheology and Water Mantle Convection and Magma Production on Present-Day Mars: The Effects of Temperature-dependent Rheology and Water

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3306l&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3306

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Scientific paper

With available geological and geophysical constraints, we explore the
mechanism of mantle convection and magma production on present-day Mars
by incorporating the effects of temperature-dependent rheology and
water.

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