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The literature on the coarse-grained inclusions of the Allende meteorite is reviewed, with attention given to petrography and major minerals, micromineralogy and microtextures, bulk chemical composition, and isotopic composition. It is concluded that the coarse-grained inclusions provide evidence for a supernova explosion that occurred just before condensation, for incompletely homogenized material from several nucleosynthetic sources, and for solar nebular regions of different chemical and isotopic composition.
Lawrence Grossman (Thu,) studied this question.