WEKO3
アイテム
{"_buckets": {"deposit": "7ffa1cb4-c2e0-43b5-97ed-5f631852dbe4"}, "_deposit": {"id": "4519", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4519"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004519", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2009-10", "bibliographicIssueDateType": "Issued"}, "bibliographicVolumeNumber": "36", "bibliographic_titles": [{"bibliographic_title": "GEOPHYSICAL RESEARCH LETTERS", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "We investigated the stress field within the Nankai accretionary prism of southwestern Japan, where very-low-frequency (VLF) earthquakes occur associated with thrust faulting. A northwest-southeast azimuth of the maximum horizontal principal stress previously estimated from borehole breakouts in wells drilled in the region by deep-sea drilling vessel Chikyu suggests trench-normal shortening, although strike-slip and normal faulting are also possible within a thrust-dominated tectonic environment. We estimated stress orientations and stress ratios by using stress tensor inversion to derive moment tensor solutions for VLF earthquakes in three regions along the Nankai Trough: off Kumano, off Muroto, and Hyuga-nada. The stress orientations we obtained indicate that the regions off Kumano and off Muroto are within a transpressional stress regime with trench-normal shortening, whereas the Hyuga-nada region on the westernmost edge of the Nankai accretionary prism is in a reverse-faulting regime. Citation: Ito, Y., Y. Asano, and K. Obara (2009), Very-low-frequency earthquakes indicate a transpressional stress regime in the Nankai accretionary prism, Geophys. Res. Lett., 36, L20309, doi:10.1029/2009GL039332.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "AMER GEOPHYSICAL UNION", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1029/2009GL039332"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1944-8007", "subitem_source_identifier_type": "EISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Yoshihiro Ito", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Youichi Asano", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Kazushige Obara", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Very-low-frequency earthquakes indicate a transpressional stress regime in the Nankai accretionary prism", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Very-low-frequency earthquakes indicate a transpressional stress regime in the Nankai accretionary prism", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4519", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4519", "relation": {}, "relation_version_is_last": true, "title": ["Very-low-frequency earthquakes indicate a transpressional stress regime in the Nankai accretionary prism"], "weko_shared_id": -1}
Very-low-frequency earthquakes indicate a transpressional stress regime in the Nankai accretionary prism
https://nied-repo.bosai.go.jp/records/4519
https://nied-repo.bosai.go.jp/records/45199a1c5e65-84de-432b-922b-5e008251709f
Item type | researchmap(1) | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|
公開日 | 2023-03-30 | |||||||||||
タイトル | ||||||||||||
言語 | en | |||||||||||
タイトル | Very-low-frequency earthquakes indicate a transpressional stress regime in the Nankai accretionary prism | |||||||||||
言語 | ||||||||||||
言語 | eng | |||||||||||
著者 |
Yoshihiro Ito
× Yoshihiro Ito
× Youichi Asano
× Kazushige Obara
|
|||||||||||
抄録 | ||||||||||||
内容記述タイプ | Other | |||||||||||
内容記述 | We investigated the stress field within the Nankai accretionary prism of southwestern Japan, where very-low-frequency (VLF) earthquakes occur associated with thrust faulting. A northwest-southeast azimuth of the maximum horizontal principal stress previously estimated from borehole breakouts in wells drilled in the region by deep-sea drilling vessel Chikyu suggests trench-normal shortening, although strike-slip and normal faulting are also possible within a thrust-dominated tectonic environment. We estimated stress orientations and stress ratios by using stress tensor inversion to derive moment tensor solutions for VLF earthquakes in three regions along the Nankai Trough: off Kumano, off Muroto, and Hyuga-nada. The stress orientations we obtained indicate that the regions off Kumano and off Muroto are within a transpressional stress regime with trench-normal shortening, whereas the Hyuga-nada region on the westernmost edge of the Nankai accretionary prism is in a reverse-faulting regime. Citation: Ito, Y., Y. Asano, and K. Obara (2009), Very-low-frequency earthquakes indicate a transpressional stress regime in the Nankai accretionary prism, Geophys. Res. Lett., 36, L20309, doi:10.1029/2009GL039332. | |||||||||||
言語 | en | |||||||||||
書誌情報 |
en : GEOPHYSICAL RESEARCH LETTERS 巻 36, 発行日 2009-10 |
|||||||||||
出版者 | ||||||||||||
言語 | en | |||||||||||
出版者 | AMER GEOPHYSICAL UNION | |||||||||||
ISSN | ||||||||||||
収録物識別子タイプ | EISSN | |||||||||||
収録物識別子 | 1944-8007 | |||||||||||
DOI | ||||||||||||
関連識別子 | 10.1029/2009GL039332 |