Tectonics of sedimentary basins in and around Japan since the opening of the Sea of Japan

Author:

Nakajima Takeshi1

Affiliation:

1. Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST)

Publisher

The Geological Society of Japan

Subject

General Earth and Planetary Sciences,General Engineering,General Environmental Science

Reference236 articles.

1. 相田 優・竹谷陽二郞・岡田尚武・長谷川四郎・丸山俊明・根本直樹(Aita, Y., Taketani, Y., Okada, H., Hasegawa, S., Maruyama, T. and Nemoto, N.), 1998, 会津地域における中新統の微化石層序と古海洋(Miocene microbiostratigraphy and paleoceanographic study of the Aizu area, Northeast Japan).福島県立博物館紀要(Bull. Fukushima Pref. Mus.), 13, 1-119.

2. Altis, S., 1999, Interpretation of a Middle Miocnene and late Quaternary steady dextral transpression in SW Japan and the opening tectonics for the Japan Sea. Tectonophysics, 302, 257-285.

3. Amano, K., 1991, Multiple collision tectonics of the South Fossa Magna in central Japan. Mod. Geol., 15, 315-329.

4. 安藤寿男(Ando, H.), 2006, 関東平野東端の太平洋岸に分布する銚子層群・那珂湊層群・大洗層の地質学的位置づけ(Geological setting of the Choshi and Nakaminato Groups and Oarai Formation exposed along the Pacific coast in the eastern end of the Kanto Plain).地質雑(Jour. Geol. Soc. Japan), 112, 84-97.

5. 青池 寛(Aoike, K.), 1999, 伊豆衝突帯の構造発達(Tectonic evolution of the Izu collision zone).神奈川県博調査研報(自然科学)(Res. Rep. Kanagawa Pref. Mus. Nat. Hist.), 9, 113-151.

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