Tom Treiman

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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. Although mid-IR spectra indicate NWA2737 is a well crystallized dunite, visible to near-IR spectra exhibit(More)
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