Discovery of Keilite in Type 3 Enstatite Chondrites: Influence of Metamorphic Temperature on Formation

Physics

Scientific paper

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Scientific paper

The discovery of keilite, previously observed in type 4-6
enstatite chondrites, in shock- or impact-melted type 3 enstatite
chondrites, constrains the post-shock equilibration temperatures
experienced by these meteorites to the range of
400°-500°C.

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