In Situ Growth of Fayalite and Hedenbergite in the Ungrouped Carbonaceous Chondrite MAC88107 with Affinities to the CM-CO Clan

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Scientific paper

The ungrouped carbonaceous chondrite MAC88107 contains secondary
fayalite (Fa90-100), hedenbergite (~Fs50Wo50), phyllosilicates,
magnetite, and Ni-bearing sulfides. Fayalite and hedenbergite formed
during aqueous alteration in an asteroidal environment.

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