Oxygen Isotopic Compostion of Ca-Fe-rich Silicates in and Around an Allende Ca-Al-rich Inclusion

Mathematics – Logic

Scientific paper

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Scientific paper

Allende Ca-Fe-rich silicates have a variable oxygen isotopic composition
along a mass fractionation trend, slightly below the TFL. Their
occurrence, texture, mineralogic and isotopic composition are better
explained by formation in a parent body setting.

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