The Significance of Fe Exchange Between Metal and Silicate Minerals in Mafic Clasts from the Howardites Kapoeta and Winterhaven

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Scientific paper

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Scientific paper

Fe in metal and silicate minerals of mafic clasts from howardites
reflects original metal composition and subsequent modifications by post
igneous processes. The sequence of exchange reactions in howardites will
elucidate the regolith history of Vesta.

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