Oxidation during metamorphism of the ordinary chondrites

Physics

Scientific paper

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Chondrites, Iron Meteorites, Metamorphism (Geology), Meteoritic Composition, Oxidation, Geophysical Fluids, Olivine, Pyroxenes, Reaction Kinetics, Meteorites, Stony Meteorites, Ordinary Chondrites, Oxidation, Iron, Metamorphism, Composition, Abundance, Olivine, Pyroxene, Metal, Heating, Thermal Effects, Fugacity, Oxygen, Mineralogy, Reduction, Temperature, Graphite, Hypotheses, Vapor, Water, H Chondrites, L Chondrites, Ll Chondrites, Parent Material

Scientific paper

It is suggested that some current concepts about the conditions of metamorphism in ordinary chondrites may be flawed. These meteorites display small systematic variations in the oxidation state of Fe. Evidence is presented that oxidation of Fe is linked to metamorphic grade in types 4-6 ordinary chondrites. This conclusion is at variance with a commonly accepted model for chondrite metamorphism that assumes Fe reduction by graphite.

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