Apatite as a Key to Evaluating the Volatile Budget of Martian Magmas: Implications from the Chassigny Meteorite

Physics

Scientific paper

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Scientific paper

In Chassigny, olivine-hosted melt inclusions contain fluor-apatite;
chlor-fluor-apatite is maskelynite-hosted, suggesting that magmatic
volatile concentrations underwent significant changes from early to late
stages of the crystallization history.

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