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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
https://doi.org/10.15083/0000032449
https://doi.org/10.15083/00000324492890c2a8-1cd5-41a0-b33d-48743106775f
名前 / ファイル | ライセンス | アクション |
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IHO83203.pdf (1.1MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2010-03-09 | |||||
タイトル | ||||||
タイトル | 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 | |||||
言語 | ja | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | Itoigawa-Shizuoka tectonic line | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | Omine-SK100 tephra | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | paleomagnetism | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | Early Pleistocene | |||||
主題Scheme | Other | |||||
キーワード | ||||||
主題 | thrust front migration | |||||
主題Scheme | Other | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15083/0000032449 | |||||
ID登録タイプ | JaLC | |||||
その他のタイトル | ||||||
その他のタイトル | Plio-Pleistocene Behavior of the Itoigawa-Shizuoka Tectonic Line in Northern Nagano Prefecture, Central Japan: Paleomagnetism of the Omine-SK110 Tephra | |||||
著者 |
植木, 岳雪
× 植木, 岳雪 |
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著者別名 | ||||||
識別子 | 123762 | |||||
識別子Scheme | WEKO | |||||
姓名 | Ueki, Takeyuki | |||||
著者所属 | ||||||
著者所属 | 独立行政法人産業技術総合研究所・地質情報研究部門 | |||||
著者所属 | ||||||
著者所属 | Institute of Geology and Geoinformation, Geological Survey of Japan, AIST | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 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. | |||||
書誌情報 |
地震研究所彙報 巻 83, 号 2, p. 163-173, 発行日 2008 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00408972 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00162258 | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
日本十進分類法 | ||||||
主題 | 51.1 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | 地震研究所 | |||||
出版者別名 | ||||||
Earthquake Research Institute, University of Tokyo |