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- W1625796522 abstract "Carbonaceous chondrites (groups CO and CV) contain three types of ferromagnesian chondrules that can be distinguished on the basis of mineralogy and texture. Statistical analysis of the bulk chemical compositions of these chondrule types suggest that two of the three types are genetically related. The chondrules in carbonaceous chondrites can thus be separated into two populations. These populations are also apparently distinct in terms of redox state and oxygen isotopic composition. The more abundant population (I) is clearly different from chondrules in unequilibrated ordinary chondrites, but the minor population (II) is similar to them in many respects. These chondrule populations may have formed by melting of solid, locally homogeneous precursor materials in different regions of the nebula, and were mixed after solidification was complete." @default.
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- W1625796522 date "1983-01-01" @default.
- W1625796522 modified "2023-09-23" @default.
- W1625796522 title "Ferromagnesian chondrules in carbonaceous chondrites" @default.
- W1625796522 hasPublicationYear "1983" @default.
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