{"created":"2023-03-30T09:20:33.896943+00:00","id":2894,"links":{},"metadata":{"_buckets":{"deposit":"a97ca50f-cc72-4a20-9194-154a2091a58e"},"_deposit":{"id":"2894","owners":[1],"pid":{"revision_id":0,"type":"depid","value":"2894"},"status":"published"},"_oai":{"id":"oai:nied-repo.bosai.go.jp:00002894","sets":[]},"author_link":[],"item_10001_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2022-09-05","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"9","bibliographicVolumeNumber":"127","bibliographic_titles":[{"bibliographic_title":"Journal of Geophysical Research: Solid Earth","bibliographic_titleLang":"en"}]}]},"item_10001_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The main cause of tsunamis is large subduction zone earthquakes with seismic magnitudes Mw?>?7, but submarine volcanic processes can also generate tsunamis. At the submarine Sumisu caldera in the Izu?Bonin arc, moderate-sized earthquakes with Mw?