Geology and paleomagnetism of the Miocene on the southern margin of the Asahi Mountains in Northeast Japan and the timing of crustal rotation

Author:

Hoshi Hiroyuki1,Yamaguchi Naoyuki1,Yoshida Takeyoshi2

Affiliation:

1. Aichi University of Education

2. Graduate School of Science, Tohoku University

Publisher

The Geological Society of Japan

Subject

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

Reference76 articles.

1. 阿部龍市・小笠原憲四郎・長澤一雄・大場 總・柳沢幸夫, 2006, 山形県小国町明沢川地域から産出したVicarya化石.山形応用地質, 26, 56–61. [Abe, R., Ogasawara, K., Nagasawa, K., Oba, S. and Yanagisawa, Y., 2006, Fossil Vicarya from the Myozawagawa area in Oguni Town in Yamagata Prefecture. Appl. Geol. Yamagata, 26, 56–61.]

2. Baba, A. K., Matsuda, T., Itaya, T., Wada, Y., Hori, N., Yokoyama, M., ...Otofuji, Y., 2007, New age constraints on counter-clockwise rotation of NE Japan. Geophys. J. Int., 171, 1325–1341.

3. Blow, W. H., 1969, Late Middle Eocene to Recent planktonic foraminiferal biostratigraphy. In Brönniman, P. and Renz, H. H., eds., Proceedings of the First International Conference on Planktonic Microfossils, Geneva, 1967, 1, E. J. Brill, Leiden, 199–422.

4. Chinzei, K., 1986, Opening of the Japan Sea and marine biogeography during the Miocene. J. Geomagn. Geoelectr., 38, 487–494.

5. 地質調査所, 1992, 100万分の1日本地質図, 第3版.工業技術院地質調査所. [Geological Survey of Japan, 1992, Geological Map of Japan, 1:1,000,000(3rd Edition). Geological Survey of Japan.]

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