{"created":"2023-07-25T10:59:06.572776+00:00","id":634,"links":{},"metadata":{"_buckets":{"deposit":"ce9854ef-5380-4403-ae07-f9b3c89d5f12"},"_deposit":{"created_by":4,"id":"634","owners":[4],"pid":{"revision_id":0,"type":"depid","value":"634"},"status":"published"},"_oai":{"id":"oai:nipr.repo.nii.ac.jp:00000634","sets":["1:314:322"]},"author_link":["14747","65312"],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1984-02","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"18","bibliographicPageStart":"13","bibliographicVolumeNumber":"15","bibliographic_titles":[{"bibliographic_title":"Memoirs of National Institute of Polar Research. Ser. C, Earth sciences"}]}]},"item_1_creator_8":{"attribute_name":"著者名(英)","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Ito, Kiyoshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Ikami, Akira","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":"The P-wave velocity structure of a part of the Prince Olav Coast, East Antarctica was revealed by a seismic refraction experiment conducted by the 21st Japanese Antarctic Research Expedition in July 1980. Ten seismic stations were set along a line with a length of about 10 km at intervals of about 1 km. The station consists of a seismometer and a direct analogue data-recorder with an electric panel-heater in an insulated box. The observed travel times of the first and later arrivals from two explosions at both ends of the line were analyzed. The P-wave velocity of the basement complex is 6.02 km/s which is a typical value in East Antarctica. This basement complex is covered by the ice sheet with the thickness of about 700-1000 m. No layer with a velocity less than 6 km/s is detected between the ice sheet and the basement complex.","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA00733470","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":"Rogional Observation Center for Earthquake Prediction,Far fculty of Science,Kyoto University"},{"subitem_text_language":"en","subitem_text_value":"Rogional Centeor Earthquake Prediction Observation,School of Science,Nagoya University"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1984-02-01"}],"displaytype":"detail","filename":"KJ00000011319.pdf","filesize":[{"value":"1.0 MB"}],"format":"application/pdf","licensetype":"license_6","mimetype":"application/pdf","url":{"label":"KJ00000011319","url":"https://nipr.repo.nii.ac.jp/record/634/files/KJ00000011319.pdf"},"version_id":"a9cd7167-6be2-4a20-9710-700af21e42b5"}]},"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":"Upper crustal structure of the Prince Olav Coast, East Antarctica","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Upper crustal structure of the Prince Olav Coast, East Antarctica","subitem_title_language":"en"}]},"item_type_id":"1","owner":"4","path":["322"],"pubdate":{"attribute_name":"公開日","attribute_value":"1984-02-01"},"publish_date":"1984-02-01","publish_status":"0","recid":"634","relation_version_is_last":true,"title":["Upper crustal structure of the Prince Olav Coast, East Antarctica"],"weko_creator_id":"4","weko_shared_id":4},"updated":"2023-07-25T14:12:48.741881+00:00"}