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Gamma-Ray Data of the Tharsis Region, Mars: A Signature of Partial Melting of the Martian Mantle?

Proceedings article published in 2008 by Mr R. El Maarry, Mj J. Toplis, O. Gasnault, D. Baratoux ORCID
This paper is available in a repository.
This paper is available in a repository.

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Abstract

A combination of GRS data and thermodynamic modeling using pMELTS is used to suggest that surface compositions determined at the Tharsis rise may represent primary melts produced by direct partial melting of the martian mantle.