Heating Experiments of the HaH 262 Eucrite and Implication for the Metamorphic History of Highly Metamorphosed Eucrites

Mathematics – Logic

Scientific paper

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Scientific paper

We performed heating experiments of a eucrite near the solidus to
understand mineralogical and chemical changes during high temperature
metamorphism. Partial melts formed at 1050-1100° C are rich in P and
Ti, suggesting preferential melting of mesostasis phases.

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