Chronostratigraphy of the Upper Miocene to Pliocene succession of the Tsubokawa Section in Shichinohe Town, Aomori Prefecture, Northeast Japan

Author:

KUDO Takashi1,YANAGISAWA Yukio1

Affiliation:

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

Publisher

National Institute of Advanced Industrial Science

Subject

General Medicine

Reference21 articles.

1. Akiba, F. (1986) Middle Miocene to Quaternary diatom biostratigraphy in the Nankai Trough and Japan Trench, and modified Lower Miocene though Quaternary diatom zones for middle-to-high latitudes of the North Pacific. In Kagami, H., Karig, D. E., Coulbourn, W. T. et al., Initial Reports of the Deep Sea Drilling Project, U. S. Government Printing Office, Washington D. C., 87, 393– 480.

2. Blow, W. H. (1969) Late Middle Eocene to Recent planktonic foraminiferal biostratigraphy. In Brönnimann, P. and Renz, H. H. eds., Proceedings of the First International Conference on Planktonic Microfossils (Geneve,1976), Leiden, no.1, 199–421.

3. Danhara, T. and Iwano, H. (2009) Determination of zeta values for fission-track age calibration using thermal neutron irradiation at the JRR-3 reactor of JAEA, Japan. Journal of Geological Society of Japan, 115, 141–145. 10.5575/geosoc.115.141

4. Danhara, T., Kasuya, M., Iwano. H. and Yamashita, T. (1991) Fission-track age calibration using internal and external surfaces of zircon. Journal of Geological Society of Japan, 97, 977–985. 10.5575/geosoc.97.977

5. Danhara, T., Iwano, H., Yoshioka, T. and Tsuruta, T. (2003) Zeta calibration values for fission track dating with a diallyl phthalate detector. Journal of Geological Society of Japan, 109, 665–668. 10.5575/geosoc.109.665

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