X-Ray Diffraction Study of Minerals from Shocked Iron Meteorites

Details X-Ray Diffraction Study of Minerals from Shocked Iron Meteorites X-Ray Diffraction Study of Minerals from Shocked Iron Meteorites

May 1966

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1966sci...152.1055l&link_type=abstract

Science, Volume 152, Issue 3725, pp. 1055-1057

Physics

7

Scientific paper

Diffraction analysis of minerals from iron meteorites indicates a pronounced shock-induced alteration in the minerals' crystallographic character. The extent of alteration seems to be dependent on the degree of shock and can therefore serve as a measure of shock intensity. The changes appear to be due to the minerals' direct recrystallization during passage of the shock wave.

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