Graphite-magnetite aggregates in ordinary chondritic meteorites

Computer Science

Scientific paper

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Chondrites, Graphite, Magnetite, Meteoritic Composition, Meteoritic Microstructures, Aggregates, Breccia, Gas-Solid Interactions, Low Temperature, Matrix Materials, Photomicrography, Regolith, X Ray Diffraction, Bremervorde Meteorite, Sharps Meteorites, Antarctic Meteorites, Alha77299, Allan Hills Meteorites, Alha77011, Alha77278, Dhajala Meteorite, Clasts, Meteorites, Graphite, Magnetite, Mineralogy, Aggregates, Experiments, Ordinary Chondrites, Crystals, Breccias, Weston Meteorite, L Chondrites, Samples,

Scientific paper

The graphite-magnetite component has been found (1) as abundant isolated inclusions in eight ordinary-chondritic, regolith breccias; (2) as the sole matrix in a new kind of unequilibrated chondrite that forms clasts in these regolith breccias; and (3) together with a Huss matrix in six unequilibrated ordinary chondrites. It is suggested that the component was formed by low-temperature, gas-solid reactions before the accretion of the meteorite, and that the isolated inclusions of graphite-magnetite in regolith breccias were derived from bodies composed of the new kind of chondrite that has graphite-magnetite as its sole matrix.

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