@article{oai:nipr.repo.nii.ac.jp:00005932,
 author = {Miyamoto, Masamichi},
 journal = {Antarctic meteorite research},
 month = {Mar},
 note = {P(論文), Raman spectra were measured for diamonds in an inclusion of the Canyon Diablo iron meteorite. The wavenumber position of a Raman peak was found in the range between 1333 and 1318cm^<-1>, and the full width at half maximum (FWHM) of the Raman peak ranges from 25 to 117cm^<-1>. These results are similar to those of Raman spectra of diamonds synthesized by shock-induced high pressure and are consistent with the consensus that diamond in Canyon Diablo formed by impact shock. No diamond grains showing a relatively narrow FWHM (7cm^<-1>) were found in the inclusion.},
 pages = {171--177},
 title = {Micro raman spectroscopy of diamonds in the Canyon Diablo iron meteorite: Implication for shock origin},
 volume = {11},
 year = {1998}
}