Raman spectrosopy of diamond in ureilite and implication for the origin of diamond

Details Raman spectrosopy of diamond in ureilite and implication for the origin of diamond Raman spectrosopy of diamond in ureilite and implication for the origin of diamond

Nov 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988georl..15.1445m&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 15, Nov. 1988, p. 1445-1448.

Physics

9

Diamonds, Geochemistry, Meteoritic Composition, Raman Spectra, Ureilites, High Temperature Environments, Minerals, Sintering

Scientific paper

Most ureilite meteorites contain diamonds that are generally thought to have been formed by shock-induced high pressure that converted carbonaceous material to diamond. Raman spectra of ureilite diamond were measured in order to investigate the origin of such diamonds. The FWHM of the Raman line at 1330/cm from diamond in the ALH-77257 ureilite is about 10/cm.

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