{"created":"2023-03-30T09:35:28.684438+00:00","id":3652,"links":{},"metadata":{"_buckets":{"deposit":"37c2d87d-02f8-49b2-b230-55832634b5e6"},"_deposit":{"id":"3652","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"3652"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00003652","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2014-06","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"372","bibliographicPageStart":"365","bibliographicVolumeNumber":"9","bibliographic_titles":[{"bibliographic_title":"Journal of Disaster Research","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The 2011 Tohoku mega-thrust earthquake caused huge crustal deformation over a wide are of Mainland Japan. Many mega-thrust earthquakes worldwide have triggered volcanic eruptions nearby, and it is assumed that stress changes due to the Tohoku earthquake resulted in a perturbation to the magma system. The objectives of our study is to evaluate this perturbation quantitatively and to analyze the mechanism of the interaction between mega-thrust earthquakes and volcanic eruptions. This paper focuses on quasi-static stress change due to viscous relaxation of a source region and the surrounding area.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_10001_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Fuji Technology Press","subitem_publisher_language":"en"}]},"item_10001_relation_14":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"10.20965/jdr.2014.p0365"}}]},"item_10001_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"1883-8030","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"E. Fujita","creatorNameLang":"ja"},{"creatorName":"E. Fujita","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"T. Kozono","creatorNameLang":"ja"},{"creatorName":"T. Kozono","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"N. Toda","creatorNameLang":"ja"},{"creatorName":"N. Toda","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"A. Kikuchi","creatorNameLang":"ja"},{"creatorName":"A. Kikuchi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Y. Ida","creatorNameLang":"ja"},{"creatorName":"Y. Ida","creatorNameLang":"en"}]}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_title":"Quasi-static stress change around Mount Fuji region due to Tohoku mega-thrust earthquake","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Quasi-static stress change around Mount Fuji region due to Tohoku mega-thrust earthquake","subitem_title_language":"ja"},{"subitem_title":"Quasi-static stress change around Mount Fuji region due to Tohoku mega-thrust earthquake","subitem_title_language":"en"}]},"item_type_id":"40001","owner":"1","path":["1670839190650"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2023-04-27"},"publish_date":"2023-04-27","publish_status":"0","recid":"3652","relation_version_is_last":true,"title":["Quasi-static stress change around Mount Fuji region due to Tohoku mega-thrust earthquake"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-04-27T05:18:30.837146+00:00"}