Mineralogy, structure and paragenesis of the products of guttogenesis due to natural aerodynamic ablation of sideritic meteorites

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Ablation, Atmospheric Entry, Meteoritic Microstructures, Aerodynamic Heating, Chemical Analysis, Meteoritic Composition, Mineralogy

Scientific paper

During atmospheric entry at high velocities, meteorites experience severe aerodynamic heating and ablation of a thin melted layer that first forms on the front surface, and later extends as a fusion crust. Tiny droplets, slags, globules and dabs are sprayed to form meteor dust. A search for the magnetic portion of such dust was performed. Information on mineralogy, chemistry, structure and texture, and paragenesis of the recovered material was gained.

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