Contrasting microstructures of fayalitic olivine in matrix and chondrules in the Allende CV3 chondrite

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Allende Meteorite, Meteoritic Composition, Olivine, Crystal Structure, Chondrule, Chondrites, Crystallinity, Microstructure, Transmission Electron Microscopy, Dehydration

Scientific paper

A detailed microstructural study using TEM of the fayalitic olivine from a variety of occurrences in the host Allende CV3 meteorite is reported. The remarkable degree of crystallinity of the olivine, absence of voids, and the fact that the fayalite invariably consists of continuous regions extending over several microns are not consistent with formation by dehydration but by some type of solid state replacement reaction.

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