{"created":"2021-03-01T06:52:27.137899+00:00","id":33647,"links":{},"metadata":{"_buckets":{"deposit":"0354c5d5-122c-409a-a3e1-46e3706b534d"},"_deposit":{"id":"33647","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"33647"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00033647","sets":["80:4535:4947:4955","9:504:4538:4949:4956"]},"author_link":["131472"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"4. 日本附近の稍深発および深発地震のメカニズム"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1965-07-15","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"52","bibliographicPageStart":"39","bibliographicVolumeNumber":"43","bibliographic_titles":[{"bibliographic_title":"東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]},"item_4_description_13":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The result of the investigation of the patterns of S waves recorded at large distances from the foci of 7 intermediate and deep earthquakes, which occurred in and near Japan, confirms the validity of the double couple hypothesis of earthquake mechanism forthese shocks. The study of the S waves of 39 additional shocks of the region recorded at De Bilt gives support to the hypothesis. The amplitude ratios of the P and S waves of these earthquakes seem to indicate that the radii of the focal spheres of earthquakes of magnitudes 6Va to 7.8 are of the order of 10 to 50km.","subitem_description_type":"Abstract"},{"subitem_description":"日本附近に起こつた7個の稍深発および深発地震について,遠距離の地点におけるS波の運動の向きの分布を調べて,これらの地震のメカニズムがdouble couoleの仮説によつて説明できることを示した.またDe Biltにおいて記録された同地域の39個の地震のS波を調べて同じ仮説が成り立つことがわかつた.マグニチュードが61/2から7.8の範囲内にあるこれらの地震のP波とS波の振幅の比から,メカニズムのモデルとして用いた震源球の半径は10kmから50km位であると推定される.","subitem_description_type":"Abstract"}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000033647","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00162258","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00408972","subitem_source_identifier_type":"ISSN"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"453","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"Royal Netherlands Meteorological Institute, De Bilt"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"RlTSEMA, A.R."}],"nameIdentifiers":[{"nameIdentifier":"131472","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-06-26"}],"displaytype":"detail","filename":"ji0431004.pdf","filesize":[{"value":"611.7 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0431004.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/33647/files/ji0431004.pdf"},"version_id":"42385341-3873-4b3f-bb78-e6b3713c2dea"}]},"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":"4. The Mechanism of Some Deep and Intermediate Earthquakes in the Region of Japan","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"4. The Mechanism of Some Deep and Intermediate Earthquakes in the Region of Japan","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["4955","4956"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2009-03-31"},"publish_date":"2009-03-31","publish_status":"0","recid":"33647","relation_version_is_last":true,"title":["4. The Mechanism of Some Deep and Intermediate Earthquakes in the Region of Japan"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T05:29:41.880436+00:00"}