X-ray diffraction study of kamacite from iron meteorites

Details X-ray diffraction study of kamacite from iron meteorites X-ray diffraction study of kamacite from iron meteorites

Jul 1968

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1968gecoa..32..773j&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 32, Issue 7, pp.773-774

Physics

2

Scientific paper

X-ray diffraction studies of kamacite ( -iron) indicate the unusual nature of its shock-induced alteration and suggest the influence of an unstable polymorph, probably -iron. Although shock-induced random disorder in kamacite can be simulated by isotropic annealing, preferred disorder apparently cannot be thus induced. The ready detection, by X-ray diffraction, of shock effects in kamacite serves to make it a useful barometer in the 130-750 kb range, particularly in cases where optical microscopy gives equivocal results.

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