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J-GLOBAL ID:201702236127976204   Reference number:17A0040802

四国西部の3種の浅海成白亜系と砕屑性ジルコンU-Pb年代スペクトル -白亜紀日本の前弧・背弧砂岩の識別-

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Material:
Volume: 125  Issue:Page: 717-745(J-STAGE)  Publication year: 2016 
JST Material Number: G0643A  ISSN: 0022-135X  CODEN: CGZAA  Document type: Article
Article type: 原著論文  Country of issue: Japan (JPN)  Language: JAPANESE (JA)
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Geological structure and tectonics  ,  Dating 
Reference (66):
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  • Aoki, K., Isozaki, Y., Kofukuda, D., Sato, T., Yamamoto, A., Maki, K., Sakata, S. and Hirata, T. (2014): Provenance diversification within an arc-trench system induced by batholith development: the Cretaceous Japan case. Terra Nova, 28, 139-149.
  • Arai, F., Hayama, Y., Hayashi, S., Hosoya, T., Ibe, H., Kanzawa, K., Kizaki, Y., Kim, G.J., Takahashi, K., Takahashi, T., Takei, K., Toya, K., Yamashita, N. and Yoshiba, K. (1963): On the Atokura conglomerate in the Shimonita district, Gumma Prefecture. Chikyu Kagaku (Earth Science), 64, 18-31.
  • Arai, H. and Takagi, H. (1998): Geotectonic development of the Atokura Nappe: Restoration of the overfold in the Shimonita area, Kanto Mountains. Journal of the Geological Society of Japan, 104, 861-876.
  • Arai, H., Murakami, S. and Takagi, H. (2000): Provenance of the Atokura Formation, Kanto Mountains, central Japan. Memoirs of the Geological Society of Japan, 56, 123-136.
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