The upper Pliocene diatom zone and fission-track age of the upper Koetoi Formation around the Sarobetsu anticline, northern Hokkaido
Author:
Affiliation:
1. Horonobe Underground Research Center, Japan Atomic Energy Agency
2. Diatom Minilab Akiba Ltd.
3. Department of Geoscience, Shimane University
Publisher
The Geological Society of Japan
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
Link
https://www.jstage.jst.go.jp/article/geosoc/112/4/112_4_284/_pdf
Reference45 articles.
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2. Akiba, F., 1986, Middle Miocene to Quaternary diatom biostratigraphy in the Nankai Trough and Japan Trench, and modified Lower Miocene through Quaternary diatom zones for middle-to-high latitudes of the North Pacific. In Kagami, H., Karig, D. E., Coulbourn, W. T. et al., Init. Repts. DSDP, 87, 393-481.
3. 秋葉文雄, 1999, 北海道天北地域の勇知層から産出したNeodenticula seminaeとProboscia curvirostris（珪藻化石）およびその生層序学的意義．地質雑, 105, 733-736．
4. 秋葉文雄・平松 力・Tsoy, I. B.・小笠原憲四郎・天野和孝, 2000, 珪藻化石によるサハリン島南部のMaruyama層・Kurasi層の年代と北海道天北地域の新第三系との対比．地学雑, 109, 203-217．
5. 秋葉文雄・一ノ関鉄郎, 1983, 北海道における新第三系の微化石層序と年代層序－特に釧路炭田南西部地域を例として－．石技誌, 48, 49-61．
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