{"created":"2023-03-31T02:23:10.694355+00:00","id":5323,"links":{},"metadata":{"_buckets":{"deposit":"5fe3165a-5e11-4566-9705-8bd8a2b84291"},"_deposit":{"id":"5323","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"5323"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00005323","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2006-06"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"1181","bibliographicPageStart":"1177","bibliographicVolumeNumber":"96","bibliographic_titles":[{"bibliographic_title":"BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The near-source energy released on a fault is estimated through the strain energy change and the fracture energy from the results of kinematic waveform inversion and dynamic modeling for two different types of earthquakes: a shallow crustal earthquake, the 2000 Tottori, Japan (M-w 6.6) earthquake, and an in-slab event, the 1999 Oaxaca, Mexico (M-w 7.5) earthquake. The procedure incorporates the spatial distribution of slip, critical slip-weakening distance, stress drop, and strength excess. The results show that the near-source energy density estimated over major asperities on the fault is nearly the same for the two earthquakes, while the fracture energy on the in-slab fault is appreciably larger than that for the crustal fault, suggesting higher strength in the in-slab fault zone. The near-source released energy on major asperities is significantly larger than the fracture energy in the two earthquakes.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"SEISMOLOGICAL SOC AMER","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.1785/0120050121"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0037-1106","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"T Mikumo","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"E Fukuyama","creatorNameLang":"en"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_title":"Near-source released energy in relation to fracture energy on earthquake faults","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Near-source released energy in relation to fracture energy on earthquake faults","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"1","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-03-30"},"publish_date":"2023-03-30","publish_status":"0","recid":"5323","relation_version_is_last":true,"title":["Near-source released energy in relation to fracture energy on earthquake faults"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-03-31T02:23:12.728476+00:00"}