On superstructure in meteoritical taenite

Details On superstructure in meteoritical taenite On superstructure in meteoritical taenite

Dec 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978metic..13..379a&link_type=abstract

(Meteoritical Society, Annual Meeting, 41st, Sudbury, Ontario, Canada, Aug. 14-17, 1978.) Meteoritics, vol. 13, Dec. 31, 1978, p

Computer Science

4

Iron Meteorites, Meteoritic Microstructures, Mineralogy, Meteoritic Composition, Neutron Diffraction, Nickel, Single Crystals, X Ray Diffraction

Scientific paper

Results of Moessbauer spectroscopy, X-ray diffraction, and neutron diffraction measurements on thin taenite lamellae of some representative iron meteorites are reviewed. The typical cloudy zone in meteoritical taenite is shown to be a consequence of the formation of a FeNi superstructure in a diffusion controlled process at temperatures below approximately 320 C.

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