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  1. 黒潮圏科学
  2. くろしお:高知大学黒潮圏研究所 所報
  3. 4

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/10126/4516
c9221c36-4ec9-42ca-a10a-f51996db1d54
名前 / ファイル ライセンス アクション
077otofuji.pdf 077otofuji.pdf (1.6 MB)
Item type 会議発表論文 / Conference Paper(1)
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
キーワード
言語 en
主題Scheme Other
主題 Rifting of continental sliver
キーワード
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
資源タイプ
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

WEKO 12014

Otofuji, Yo-ichiro

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Matsuda, Takaaki

× Matsuda, Takaaki

WEKO 12015

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
ISSN
収録物識別子タイプ ISSN
収録物識別子 09131302
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN1020384X
フォーマット
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
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Cite as

Otofuji, Yo-ichiro, Matsuda, Takaaki, 1989, Amounts of clockwise rotation of southwest Japan ―Fan shape opening of thesouthwestern part of the Japan Sea―: 高知大学黒潮圏研究所, 77–93 p.

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