Mineralogy and Petrology of Al-rich Objects in the CH Carbonaceous Chondrite North West Africa 739

Physics

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Scientific paper

The CH CAIs are dominated by the high-T mineral assemblages (hibonite,
grossite, perovskite, and gehlenitic melilite), they must have been
efficiently isolated from the hot nebular region, like some chondrules
and the zoned Fe,Ni-metal grains of CHs.

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