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Amounts of clockwise rotation of southwest Japan ―Fan shape opening of thesouthwestern part of the Japan Sea―
http://hdl.handle.net/10126/4516
http://hdl.handle.net/10126/4516c9221c36-4ec9-42ca-a10a-f51996db1d54
名前 / ファイル | ライセンス | アクション |
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Item type | 会議発表論文 / Conference Paper(1) | |||||
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公開日 | 2010-05-12 | |||||
タイトル | ||||||
タイトル | Amounts of clockwise rotation of southwest Japan ―Fan shape opening of thesouthwestern part of the Japan Sea― | |||||
言語 | en | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Paleomagnetism | |||||
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言語 | en | |||||
主題Scheme | Other | |||||
主題 | Rifting of continental sliver | |||||
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言語 | en | |||||
主題Scheme | Other | |||||
主題 | Japan Sea | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Rotation | |||||
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資源タイプ識別子 | http://purl.org/coar/resource_type/c_5794 | |||||
資源タイプ | conference paper | |||||
著者 |
Otofuji, Yo-ichiro
× Otofuji, Yo-ichiro× Matsuda, Takaaki |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Paleomagnetic measurements have been carried out on welded tuffs ranging in age between 58 Ma and 112 Ma from Yamaguchi and Go river areas in the central part of Southwest Japan. The new data, together with those of younger igneous rocks published previously, define the change of paleomagnetic field direction during the late Mesozoic/Cenozoic period for Southwest Japan. The paleomagnetic direction from this area has pointed 56±3° clockwise from the expected field direction estimated from APWP (apparent polar wandering path) of the whole of Eurasia during the period between 100 and 20 Ma. In comparison with the expected one from the eastern margin of Eurasia (Korea, China, Siberia), the Cretaceous field direction of Southwest Japan shows the clockwise deflection by 44-49°. These results establish that while the eastern margin of Eurasia, including Southwest Japan, was rotated more or less with respect to the main part of Eurasia during last 100 Ma, Southwest Japan was rotated clockwise through more than 40° with respect to the eastern margin of Eurasia since 20 Ma. The large amount of rotation for Southwest Japan implies that it is rotated by an opening of the southwestern part of the Japan Sea, which widens northeastward (fan shape opening). The tectonic feature of Southwest Japan and the Japan Sea is analogous to that of Corso-Sardinia and the Ligurian Sea in the Mediterranean, indicating that the fan shape opening is a specific feature of the rifting of the continental sliver at the continental rim. | |||||
内容記述 | ||||||
内容記述タイプ | Other | |||||
内容記述 | Japanese WESTPAC Symposium. June 6-7, 1989. Ocean Research Institute, University of Tokyo. 西太平洋におけるマイクロプレートテクトニクスと古環境地図に関する研究会. 1989年6月6日-7日. 東京大学海洋研究所. | |||||
書誌情報 |
くろしお. 特別号 : 高知大学黒潮圏研究所所報 = Report of the Institute of the Kuroshio Sphere, Kochi University. Special series 巻 4, p. 77-93, 発行日 1989-12-20 |
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収録物識別子タイプ | ISSN | |||||
収録物識別子 | 09131302 | |||||
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収録物識別子タイプ | NCID | |||||
収録物識別子 | AN1020384X | |||||
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内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
出版者 | ||||||
出版者 | 高知大学黒潮圏研究所 | |||||
言語 | ja |