{"_buckets": {"deposit": "1e11d8fc-6dcd-48e7-9c34-b7894cb2d93c"}, "_deposit": {"id": "4413", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4413"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004413", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2002-09"}, "bibliographicIssueNumber": "1-4", "bibliographicPageEnd": "52", "bibliographicPageStart": "41", "bibliographicVolumeNumber": "355", "bibliographic_titles": [{"bibliographic_title": "TECTONOPHYSICS", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Knowledge of the crustal structure, especially the geometry of seismogenic faults, is key to understanding active tectonic processes and assessing the size and frequency of future earthquakes. To reveal the relationship between crustal structure and earthquake activity in northern Honshu Island, common midpoint (CMP) deep reflection profiling and earthquake observations by densely deployed seismic stations were carried Out across S the active reverse faults that bound the Ou Backbone range. The 40-km-long CMP profile. portray a relatively simple fault geometry within the seismogenic layer. The reverse faults merge at a midcrustal detachment just below the base of the seismogenic layer, producing a pop-up structure that forms the On Backbone range. The top of the reflective middle to lower crust (4.5 s in travel time (TWT)) nearly coincides with the bottom of seismogenic layer. The P-wave velocity structure and surface geology suggest that the bounding faults are Miocene normal faults that have been reactivated as reverse faults. (C) 2002 Elsevier Science B.V. All rights reserved.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "ELSEVIER SCIENCE BV", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1016/S0040-1951(02)00133-6"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0040-1951", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "H Sato", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "N Hirata", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "T Iwasaki", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "M Matsubara", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "T Ikawa", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Deep seismic reflection profiling across the Ou Backbone range, northern Honshu Island, Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Deep seismic reflection profiling across the Ou Backbone range, northern Honshu Island, Japan", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4413", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "4413", "relation": {}, "relation_version_is_last": true, "title": ["Deep seismic reflection profiling across the Ou Backbone range, northern Honshu Island, Japan"], "weko_shared_id": -1}