Petrology of types 4-6 carbonaceous chondrites

Mathematics – Logic

Scientific paper

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Carbonaceous Chondrites, Metamorphism (Geology), Meteoritic Composition, Mineralogy, Petrology, Calcium Oxides, Chondrule, Fayalite, Meteoritic Microstructures, Olivine, Oxygen Isotopes, Meteorites, Carbonaceosu Chondrites, Samples, Meteorite, Petrology, Coolidge, Karoonda, Pca Meteorites, Pca82500, Classification, Mulga, Comparisons, Ll6 Chondrites, C Chondrites, Yamato 6903, Composition, Matrix, Mineralogy, Fugacity, Oxygen, Metamorphism, Abundance, Metal, Parent Bodies, Cv3 Chondrites, Ordinary Chondrite

Scientific paper

A comparative mineralogic study has been made of Coolidge, Karoonda, and new C4 chondrites in order to clarify the origin of C4-6 chondrites. It is shown that the properties of all C4-6 chondrites are consistent with an origin by metamorphism of C3-like precursors by processes analogous to those operating in ordinary chondrite parent bodies or planetesimals. However, type 4-6 material was not well mixed with type 3 material in the CV3 parent body. It is concluded that C4-6 chondrites may come from one or more separate parent bodies.

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