Magnetic anisotropy and porosity of chondrites

Physics

Scientific paper

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Anisotropy, Chondrites, Magnetic Permeability, Metamorphism (Geology), Meteoritic Composition, Porosity, Carbonaceous Chondrites, Correlation, Meteorite Collisions, Meteoritic Microstructures, Radioactive Age Determination, Shock Heating, Meteorites, Chrondrites, Porosity, Anisotropy, Magnetic Properties, Ages, Classification, E Chondrites, H Chrondrites, L Chondrites, Ll Chondrites, Comparisons, Metamorphism, Dating Techniques, Potassium, Argon, Impacts, Experiments, Data, Intensity, Petrology, Sources, Or

Scientific paper

The measured magnetic anisotropy and porosity of various chondrites are found to be inversely correlated when they are considered by class of chondrites (E, H and L + LL). For chondrites with similar porosities, the anisotropies for H and E chondrites are smaller than for L and LL chondrites, which have lower metal contents. The anisotropy and porosity are not dependent on the metamorphic grade of chondrites. K-Ar ages of strongly anisotropic and/or less porous chondrites are younger than those of less anisotropic and/or more porous chondrites. These observations suggest that impacts which reset the K-Ar ages produced the anisotropy and reduced the porosity of chondrites.

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