Identification and correlation of tephras from the Plio-Pleistocene Shobudani Group, Kinokawa River, southwest Japan-Reference-Cited by-同舟云学术

Identification and correlation of tephras from the Plio-Pleistocene Shobudani Group, Kinokawa River, southwest Japan

Published:2018-12-01 Issue:6 Volume:57 Page:211-227
ISSN:0418-2642
Container-title:The Quaternary Research (Daiyonki-Kenkyu)
language:en
Short-container-title:Daiyonki-kenkyu

Author:

Maruyama Seiji¹,Takemura Keiji²,Hirata Takafumi³,Iwano Hideki¹,Yamashita Tohru¹,Danhara Tohru¹

Affiliation:

1. Kyoto Fission-Track Co.

2. Institute for Geothermal Sciences, Graduate School of Science, Kyoto University

3. Department of Geology and Mineralogy, Faculty of Science, Kyoto University

Publisher

Japan Association for Quaternary Research

Subject

General Earth and Planetary Sciences,General Environmental Science

Link

https://www.jstage.jst.go.jp/article/jaqua/57/6/57_211/_pdf

Reference67 articles.

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3. Danhara, T., Yamashita, T., Iwano, H., Takemura, K. and Hayashida, A. (2010) Chronology of the 1400-m core obtained from Lake Biwa in 1982-1983 : Re-investigation of fission-track ages and tephra identification. The Quaternary Research (Daiyonki-kenkyu), 49, 101-119. (J+E)

4. Disaster Prevention Research Institute and Kyoto University (2015) Accomplishment report (FY2014) of comprehensive research on the Median Tectonic Line (Kongo-Izumi segments). http://www.jishin.go.jp/main/chousakenkyuu/mlt_juten/h26/index.htm, Retrieved April 6, 2018. (J)

5. Galbraith, R.F. (1981) On statistic models for fission track counts. Mathematical Geosciences, 13, 471-488.

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