Oceanic rocks between the Mikabu Greenstones and the Kashiwagi Unit of the Northern Chichibu Belt in the eastern margin of the Kanto Mountains, and discussion of klippe theory

Author:

Hara Hidetoshi1,Tominaga Kohei2

Affiliation:

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

2. Geopark Office, City of Tsukuba

Publisher

The Geological Society of Japan

Subject

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

Reference51 articles.

1. Endo, S. and Wallis, S. R., 2017, Structural architecture and low-grade metamorphism of the Mikabu-Northern Chichibu accretionary wedge. J. Metamor. Geol., 35, 695–716.

2. 遠藤俊祐・横山俊治, 2019, 本山地域の地質.地域地質研究報告(5万分の1地質図幅).産総研地質調査総合センター.100p. [Endo, S. and Yokoyama, S., 2019, Geology of the Motoyama District. Quadrangle Series, 1: 50,000, Geol. Surv. Japan, AIST, 100p.]

3. Ernst, W. G., 1972, Possible Permian oceanic crust and plate junction in central Shikoku, Japan. Tectonophysics, 15, 233–239.

4. Fujimoto(Hujimoto), H., 1936, Stratigraphic and palaeontological studies of Titibu System of the Kwanto Mountainland, part 1 Stratigraphy. Sci. Rep., Tokyo Bunrika Daigaku, Sec. C, 1, 157–188.

5. Fujimoto(Hujimoto), H., 1937, The nappe theory with reference to the north-eastern part of the Kwanto Mountnainland. Sci. Rep., Tokyo Bunrika Daigaku, Sec. C, 1, 215–243.

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