Late Miocene–mid-Pliocene tectonically induced formation of the semi-closed Japan Sea, inferred from seawater Nd isotopes-Reference-Cited by-同舟云学术

Late Miocene–mid-Pliocene tectonically induced formation of the semi-closed Japan Sea, inferred from seawater Nd isotopes

Published:2018-09-11 Issue:10 Volume:46 Page:903-906
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:

Author:

Kozaka Yukiko¹,Horikawa Keiji²,Asahara Yoshihiro³,Amakawa Hiroshi⁴,Okazaki Yusuke⁵

Affiliation:

1. Graduate School of Science and Engineering for Education, University of Toyama, Gofuku 3190, Toyama 930-8555, Japan

2. Graduate School of Science and Engineering for Research, University of Toyama, Gofuku 3190, Toyama 930-8555, Japan

3. Department of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8601, Japan

4. Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15, Natsushima-cho, Yokosuka-shi, Kanagawa 237-0061, Japan

5. Department of Earth and Planetary Sciences, Graduate School of Sciences, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka 819-0395, Japan

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/geology/article-pdf/46/10/903/4338769/903.pdf

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