{"created":"2021-03-01T06:51:07.313046+00:00","id":32449,"links":{},"metadata":{"_buckets":{"deposit":"ff231c6c-6de6-4d6b-83ac-a95d35e383d3"},"_deposit":{"id":"32449","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32449"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032449","sets":["80:4535:4579:4583","9:504:4538:4581:4584"]},"author_link":["123762","123761"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Plio-Pleistocene Behavior of the Itoigawa-Shizuoka Tectonic Line in Northern Nagano Prefecture, Central Japan: Paleomagnetism of the Omine-SK110 Tephra"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2008","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"173","bibliographicPageStart":"163","bibliographicVolumeNumber":"83","bibliographic_titles":[{"bibliographic_title":"地震研究所彙報"}]}]},"item_4_description_13":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"This study aims to reveal Late Pliocene to Early Pleistocene geomorphic and structural evolution of the Omine Belt, North Fossa Magna, central Japan, associated with tectonic movement of the Itoigawa-Shizuoka tectonic line.  A comparison of the paleomagnetic directions of a distinct wide-spread tephra, which is exposed in different areas, is useful to detect tectonic rotation because it gives instantaneous paleomagnetic directions from proximal to distal areas.  The Omine-SK110 tephra with an estimated age of 1.65－1.60Ma is distributed in the Omine Belt as Omine Welded Tuff and in the west Tama Hills of the Kanto Plain as a co-ignimbrite of the Horinouchi 2 Tuff.  Pro-gressive alternating field and thermal demagnetization experiments reveal that both tephras have reversed paleomagnetic directions that are almost identical to each other.  As the west Tama Hills had been in a tectonically stable area since Late Pliocene, there might be no vertical-axis rotation in the Omine Belt.  Thus, the Omine Belt would not be a pull-apart basin with left-lateral strike-slip faulting between the Otari-Nakayama fault and the active fault system of the Itoigawa-Shizuoka tectonic line.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"123762","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Ueki, Takeyuki"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000032449","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00162258","subitem_source_identifier_type":"NCID"}]},"item_4_source_id_8":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"00408972","subitem_source_identifier_type":"ISSN"}]},"item_4_subject_15":{"attribute_name":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"51.1","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"独立行政法人産業技術総合研究所・地質情報研究部門"},{"subitem_text_value":"Institute of Geology and Geoinformation, Geological Survey of Japan, AIST"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"植木, 岳雪"}],"nameIdentifiers":[{"nameIdentifier":"123761","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-06-26"}],"displaytype":"detail","filename":"IHO83203.pdf","filesize":[{"value":"1.1MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"IHO83203.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32449/files/IHO83203.pdf"},"version_id":"d588e71c-c037-4767-a721-cb6349cd1579"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Itoigawa-Shizuoka tectonic line","subitem_subject_scheme":"Other"},{"subitem_subject":"Omine-SK100 tephra","subitem_subject_scheme":"Other"},{"subitem_subject":"paleomagnetism","subitem_subject_scheme":"Other"},{"subitem_subject":"Early Pleistocene","subitem_subject_scheme":"Other"},{"subitem_subject":"thrust front migration","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"長野県北部，糸魚川―静岡構造線の鮮新世以降の活動様式: 大峰―SK110テフラの古地磁気方位に基づいて","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"長野県北部，糸魚川―静岡構造線の鮮新世以降の活動様式: 大峰―SK110テフラの古地磁気方位に基づいて","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"1","path":["4583","4584"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2010-03-09"},"publish_date":"2010-03-09","publish_status":"0","recid":"32449","relation_version_is_last":true,"title":["長野県北部，糸魚川―静岡構造線の鮮新世以降の活動様式: 大峰―SK110テフラの古地磁気方位に基づいて"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:08:28.296570+00:00"}