{"_buckets": {"deposit": "b24c4e7e-144a-4dda-8177-e9cd7ce6bb5c"}, "_deposit": {"id": "4623", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4623"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004623", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2010-07", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "7", "bibliographicPageEnd": "500", "bibliographicPageStart": "496", "bibliographicVolumeNumber": "3", "bibliographic_titles": [{"bibliographic_title": "NATURE GEOSCIENCE", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Southwestern Japan lies at the boundary between the subducting Philippine Sea plate and the overriding Eurasian plate. A magnitude 8 megathrust earthquake ruptured the Tonankai and Nankai segments in 1944 and 1946, respectively, but the neighbouring Tokai segment of the plate boundary remained locked(1). A large megathrust earthquake in the Tokai region has therefore been expected. In 2009, a magnitude 6.4 earthquake took place in Suruga Bay, within the Philippine Sea subducting plate, close to the Tokai segment. Here, we use a fault-slip model to examine the impact of the stress changes(2) caused by the Suruga Bay event on the Tokai segment. We show that the occurrence rate of plate-boundary seismicity increased following the earthquake. Most of the presumed strongly locked patches of the Tokai segment are located within areas of increased stress. Rupturing of a locked patch-following a threshold level of seismic stress-could trigger the rupture of the entire Tokai segment, leading to a megathrust earthquake.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "NATURE PUBLISHING GROUP", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1038/NGEO885"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1752-0908", "subitem_source_identifier_type": "EISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "S. Aoi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "B. Enescu", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "W. Suzuki", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Y. Asano", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "K. Obara", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "T. Kunugi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "K. Shiomi", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Stress transfer in the Tokai subduction zone from the 2009 Suruga Bay earthquake in Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Stress transfer in the Tokai subduction zone from the 2009 Suruga Bay earthquake in Japan", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4623", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4623", "relation": {}, "relation_version_is_last": true, "title": ["Stress transfer in the Tokai subduction zone from the 2009 Suruga Bay earthquake in Japan"], "weko_shared_id": -1}