Evolution of the Martian Mantle and Crust. A Crystal Chemical Perspective from Olivine in Basaltic Shergottites

Details Evolution of the Martian Mantle and Crust. A Crystal Chemical Perspective from Olivine in Basaltic Shergottites Evolution of the Martian Mantle and Crust. A Crystal Chemical Perspective from Olivine in Basaltic Shergottites

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3072s&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3072

Physics

Scientific paper

Here, we constrain the physical mechanisms by which shergottites obtain
their compositional characteristics through a major and trace element
study of one of the earliest crystallizing phases (olivine) in some of
the more primitive shergottites.

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