Al-rich Clinopyroxenes in the CH Chondrite NWA 470: Condensates from Fractionated Nebular Systems

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Scientific paper

Clinopyroxenes with very different Al2O3 contents coexist in two CAIs
and a euhedral pyroxene grain of the CH chondrite NWA 470. These
clinopyroxenes apparently formed by condensation from fractionated
nebular systems.

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