Formation Process of Quenched Angrites Inferred from Deformed Olivine Xenocrysts in Gadamis 010

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Hayashi H.* Honda R. Mikouchi T. Yamaguchi A.

METSOC 2026 abstract (PDF)

“Gadamis 010 contains olivine xenocrysts and some shows mosaic texture with little Fe-Mg zoning but variable Ca content. This supports the “hot shock” hypothesis for quenched angrites, while indicating different thermal conditions from known samples.”

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