Stratigraphic revision of the Miocene“ Saikawa Formation” distributed in the southern Kanazawa area, Ishikawa Prefecture, central Japan.
Author:
Affiliation:
1. School of Natural System, College of Science and Engineering, Kanazawa University
2. AIST, Geological Survey of Japan, Research Institute of Geology and Geoinformation
Publisher
National Institute of Advanced Industrial Science
Subject
General Medicine
Link
https://www.jstage.jst.go.jp/article/bullgsj/68/5/68_183/_pdf
Reference23 articles.
1. 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., Initial Reports of the Deep Sea Drilling Project, U. S. Goverment Printing Office, Washington D. C., 87, 393– 480.
2. Gradstein, F. M., Ogg, J. M., Schmitz, M. D. and Ogg, G. M.(2012) The Geologic Time Scale 2012. 1144p. Elsevier, Amsterdam, Boston.
3. Fossil Boring Shells found on the Unconformable Surface below the Omma Formation (Pliocene) near Kanazawa City, Japan.,
4. The lower unconformity and molluscan fossils of the basal part of the early Pleistocene Omma Formation at its type section, Ishikawa Prefecture, central Japan.
5. Kitamura, A. and Kimoto, K. (2007) Eccentricity cycles shown by early Pleistocene planktonic foraminifers of the Omma Formation, Sea of Japan. Glob. Planet. Change, 55, 273–283. 10.1016/j.gloplacha.2006.09.001
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