Correlation between the Obama Formation of the Inubou Group in the Choshi district and the Kiwada, Otadai and Umegase Formations of the Kazusa Group in the Boso Peninsula, central Japan, based on key tephra layers-Reference-Cited by-同舟云学术

Correlation between the Obama Formation of the Inubou Group in the Choshi district and the Kiwada, Otadai and Umegase Formations of the Kazusa Group in the Boso Peninsula, central Japan, based on key tephra layers

Published:2004 Issue:8 Volume:110 Page:480-496
ISSN:0016-7630
Container-title:The Journal of the Geological Society of Japan
language:en
Short-container-title:Jour. Geol. Soc. Japan

Author:

Fujioka Michiaki¹,Kameo Koji²

Affiliation:

1. Department of Earth Sciences, Faculty of Science, Chiba University

2. Marine Biosystems Research Center, Chiba University, c/o Department of Earth Sciences, Faculty of Science, Chiba 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/110/8/110_8_480/_pdf

Reference29 articles.

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3. 藤岡導明・小竹信宏, 2003, テフラ鍵層に基づく上総層群大田代層・梅ヶ瀬層と豊房層群加茂層との対比. 第四紀研究, 42, 375-387.

4. 久光敏夫・岡田誠, 1997, 銚子地域第四系犬吠層群中部の火山灰層を用いた上総層群との直接対比. 日本地質学会第104年学術大会講演要旨, 370.

5. 亀尾浩司・佐藤時幸, 1999, 石灰質ナンノ化石層序の最近の知見とその応用—とくに常磐海域坑井の新第三系・第四系層序について—. 石技誌, 64, 17-27.

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