Martian magmatism from plume metasomatized mantle
Abstract
Direct analysis of the composition of Mars is possible through delivery of meteorites to Earth. Martian meteorites include ∼165 to 2400 Ma shergottites, originating from depleted to enriched mantle sources, and ∼1340 Ma nakhlites and chassignites, formed by low degree partial melting of a depleted mantle source. To date, no unified model has been proposed to explain the petrogenesis of these distinct rock types, despite their importance for...
Paper Details
Title
Martian magmatism from plume metasomatized mantle
Published Date
Nov 15, 2018
Journal
Volume
9
Issue
1
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