Three Distinct Shallow Marine Cretaceous Units in Western Shikoku and the U–Pb Age Spectra of Their Detrital Zircons:-Reference-Cited by-同舟云学术

Three Distinct Shallow Marine Cretaceous Units in Western Shikoku and the U–Pb Age Spectra of Their Detrital Zircons:

Published:2016 Issue:5 Volume:125 Page:717-745
ISSN:0022-135X
Container-title:Journal of Geography (Chigaku Zasshi)
language:en
Short-container-title:Journal of Geography(Chigaku Zasshi)

Author:

NAKAHATA Hiroki¹,ISOZAKI Yukio¹,TSUTSUMI Yukiyasu²

Affiliation:

1. Department of Earth Science and Astronomy, The University of Tokyo

2. Department of Geology and Paleontology, National Museum of Nature and Science

Publisher

Tokyo Geographical Society

Subject

Earth-Surface Processes,Geology,Geophysics,Geography, Planning and Development,Global and Planetary Change

Link

https://www.jstage.jst.go.jp/article/jgeography/125/5/125_125.717/_pdf

Reference64 articles.

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2. 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.

3. 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.

4. 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.

5. 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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