Seven polycrystalline iron meteorites (Forsyth County, Holland's Store, Wathena, Pima Co., Chico Mountains, Kopjes Vlei and Mejillones), of bulk composition as normal hexahedrites of group II A, are shown to be severely altered hexahedrites. Mic-roprobe examination and various heat treatments of synthetic alloys support the conclusion that the meteorites after a primary slow cooling were subjected to shock-reheating above 800°C. Thereby the following transformations took place a-α-γ->α 2 ->α, and an unequilibrated structure, very sensitive to grain-boundary corrosion was formed.
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Open AccessHaloalkane-Aromatic Complexes in the Ground and Excited States Molecular Orbital CalculationJune 2, 2014
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Open AccessWhen do Projections Commute?June 2, 2014
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Open AccessVibrational Total Energy Distributions in Terms of Symmetry Coordinates, Forces and MomentaJune 2, 2014