High-Magnesian Olivine in the Argyre Rim: Derived from a Primitive Magma?

Details High-Magnesian Olivine in the Argyre Rim: Derived from a Primitive Magma? High-Magnesian Olivine in the Argyre Rim: Derived from a Primitive Magma?

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.2094l&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.2094

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Scientific paper

High-Mg olivine (Fo80-90) units are mapped within the Argyre basin
as part of an eroded annulus (uplifted basin rim). This high-Mg olivine,
plus other minerals present, may represent primitive martian
mantle-derived material similar to Y-980459.

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