Are Megacrysts in Olivine-Phyric Shergottites Xenocrysts, Phenocrysts, or Something Else?

Physics

Scientific paper

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Scientific paper

We argue based on detailed analyses and modeling of shergottite LAR
06319 that its olivines are antecrysts, formed from a melt similar to
the current groundmass and entrained from a cumulate pile prior to
eruption.

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