{"created":"2021-03-01T06:51:32.722534+00:00","id":32829,"links":{},"metadata":{"_buckets":{"deposit":"48aa6c1a-23ed-4461-a353-a34413455540"},"_deposit":{"id":"32829","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32829"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032829","sets":["80:4535:4747:4755","9:504:4538:4749:4756"]},"author_link":["127843","127842"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Relation between Seismic Intensity near the Epicenter, Focal Depth and Magnitude"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1988-06-30","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"31","bibliographicPageStart":"23","bibliographicVolumeNumber":"63","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":"日本の地震について,震央付近の震度I0(気象庁震度階級),マグニチュードM(気象庁方式),震源の深さh(km)の標準的関係を表す実験式を1114個の震度データを用いて求め,次式を得た.M=0.23 I0+0.105 I02+1.2log h+1.3この式はMが2～8,hがO～100km.I0がO～6の地震を対象としている.ただしh=Oと発表されている地震の実際の深さは数kmと考えて,h<3kmの場合はh=3kmと置く,Mが5程度より大きい地震についてはm=1.2I0+1.21log h-0.83すなわちI0=O.83 M-log h+0.71を用いてもよい.","subitem_description_type":"Abstract"},{"subitem_description":"An empirical formula for the seismic intensity (JMA scale) I0 near the epicenter of an earthquake of magnitude M and focal depth h has been determined using 1114 data on seismic intensity recorded in Japan. The formula has the form M=0.23I0+O.105I02+1.2 log h+1.3 for M=2～8, h=3～100km, and I0≧0. For larger earthquakes (M=5～8), this formula is almost equivalent to M=1.2I0+1.2log h-0.83.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"127843","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Utsu, Tokuji"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000032829","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":"地震研究所"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"宇津, 徳治"}],"nameIdentifiers":[{"nameIdentifier":"127842","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":"ji0631002.pdf","filesize":[{"value":"479.1 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0631002.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32829/files/ji0631002.pdf"},"version_id":"d8ce996c-f150-46ce-9183-0978c4c90c72"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"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":"震央付近の震度-震源の深さ-マグニチュードの関係","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"震央付近の震度-震源の深さ-マグニチュードの関係","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"1","path":["4755","4756"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-05-30"},"publish_date":"2008-05-30","publish_status":"0","recid":"32829","relation_version_is_last":true,"title":["震央付近の震度-震源の深さ-マグニチュードの関係"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:08:46.764348+00:00"}