Miocene strata and the August 2022 heavy rain disaster in the southwestern part of Yamagata Prefecture in Northeast Japan
Author:
Affiliation:
1. Aichi University of Education
2. Faculty of Science, Yamagata University
Publisher
The Geological Society of Japan
Link
https://www.jstage.jst.go.jp/article/geosoc/130/1/130_2024.0018/_pdf
Reference70 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. 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., eds., Init. Rep. DSDP, 87, U.S. Govern. Print. Office, Washington, DC, 393–480.
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, Vol. 1, E. J. Brill, Leiden, 199–421.
4. Chinzei, K., 1986, Opening of the Japan Sea and marine biogeography during the Miocene. J. Geomagn. Geoelec., 38, 487–494.
5. Fournier, M., Jolivet, L. and Fabbri, O., 1995, Neogene stress field in SW Japan and mechanism of deformation during the Sea of Japan opening. J. Geophys. Res., 100, 24295–24314.
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