{"created":"2023-07-25T11:03:06.904486+00:00","id":5932,"links":{},"metadata":{"_buckets":{"deposit":"909783f7-50cc-4e91-879a-5e23d3229e00"},"_deposit":{"created_by":4,"id":"5932","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"5932"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00005932","sets":["1259:1260:1264:773:775"]},"author_link":["9861"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1998-03","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"177","bibliographicPageStart":"171","bibliographicVolumeNumber":"11","bibliographic_titles":[{"bibliographic_title":"Antarctic meteorite research"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Miyamoto, Masamichi","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"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.","subitem_description_type":"Other"}]},"item_1_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15094/00005932","subitem_identifier_reg_type":"JaLC"}]},"item_1_publisher_22":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"National Institute of Polar Research"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA11182426","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Mineralogical Institute, Graduate School of Science, University of Tokyo"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1998-03-01"}],"displaytype":"detail","filename":"KJ00000040924.pdf","filesize":[{"value":"710.3 kB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000040924","url":"https://nipr.repo.nii.ac.jp/record/5932/files/KJ00000040924.pdf"},"version_id":"15b4334c-e76d-4139-808c-257df8769f34"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Micro raman spectroscopy of diamonds in the Canyon Diablo iron meteorite: Implication for shock origin","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Micro raman spectroscopy of diamonds in the Canyon Diablo iron meteorite: Implication for shock origin"}]},"item_type_id":"1","owner":"4","path":["775"],"pubdate":{"attribute_name":"公開日","attribute_value":"1998-03-01"},"publish_date":"1998-03-01","publish_status":"0","recid":"5932","relation_version_is_last":true,"title":["Micro raman spectroscopy of diamonds in the Canyon Diablo iron meteorite: Implication for shock origin"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T12:08:27.534897+00:00"}