The Tishomingo Iron: Relationship to IVB Irons, CR Clan Chondrites, and Angrites and Implications for the Origin of Volatile-depleted Iron Meteorites

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Scientific paper

The oxygen isotopic and siderophile element composition of Tishomingo
suggest formation through melting of a CR-like precursor through
processes similar to IVB irons, but on a separate parent body. A direct
link with angrites is possible.

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