Correlation between Marine isotope stages and Middle to late Pleistocene marine deposits inferred from electric conductivity analysis in the Tokushima Plain, Shikoku Island, western Japan-Reference-Cited by-同舟云学术

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Correlation between Marine isotope stages and Middle to late Pleistocene marine deposits inferred from electric conductivity analysis in the Tokushima Plain, Shikoku Island, western Japan

Published:2024-05-01 Issue:2 Volume:63 Page:147-157
ISSN:0418-2642
Container-title:The Quaternary Research (Daiyonki-Kenkyu)
language:en
Short-container-title:The Quaternary Res.

Author:

Sato Yoshiki¹,Hongo Misao²,Mizuno Kiyohide¹

Affiliation:

1. AIST Geological Survey of Japan, Research Institute of Geology and Geoinformation

2. Alps Technical Research Laboratory Co. Ltd

Publisher

Japan Association for Quaternary Research

Link

https://www.jstage.jst.go.jp/article/jaqua/63/2/63_63.2222/_pdf

Reference54 articles.

1. 阿子島　功・須鎗和巳（1989）中央構造線吉野川地溝の形成過程．地球科学，43，428-442.

2. Fujiki, T., Morita, Y. and Miyoshi, N. (1998) Vegetational history of the area around Kashira Island in the Inland Sea, Okayama Prefecture, western Japan. Quarterly Journal of Geography, 50, 189-200, doi: 10.5190/TGA.50.189.

3. 古田　昇（2005）平野の環境歴史学．268 p，古今書院．

4. Furutani, M. (1989) Stratigraphical subdivision and pollen zonation of the Middle and Upper Pleistocene in the Coastal Area of Osaka Bay, Japan. Journal of Geosciences, Osaka City University, 32, 91-121.

5. 本郷美佐緒（2009）大阪堆積盆地における中部更新統の花粉生層序と古環境変遷．地質学雑誌，115，64-79.

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