Zircon U-Pb age of the acidic tuff from the Miocene Kuma Group, western Shikoku
Author:
Affiliation:
1. Tokyo Keizai University
2. Graduate School of Earth and Environmental Sciences, Hirosaki University
Publisher
The Geological Society of Japan
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
Link
https://www.jstage.jst.go.jp/article/geosoc/127/10/127_2021.0020/_pdf
Reference33 articles.
1. Chiba, E. and Sakakibara, M., 2006, Peperite at boundary between Middle Miocene andesitic lava and clastic sediments, western Shikoku, Japan. J. Geol. Soc. Japan, 112, XIX–XX.
2. Hanzawa, S., 1959, The foraminiferal species Fabiania cassis（Oppenheim）in Japan. Contrib. Cushman Found. Foraminifera Res., 10, 119–122.
3. 星 博幸, 2018, 中新世における西南日本の時計回り回転．地質雑, 124, 675–691. ［Hoshi, H., 2018, Miocene clockwise rotation of Southwest Japan. J. Geol. Soc. Japan, 124, 675–691.］
4. Hoshi, H., Kato, D., Ando, Y. and Nakashima, K., 2015, Timing of clockwise rotation of Southwest Japan: constraints from new middle Miocene paleomagnetic results. Earth Planets Space, 67, 92, doi: 10.1186/s40623-015-0266-3.
5. Iwano, H., Orihashi, Y., Hirata, T., Ogasawara, M., Danhara, T., Horie, K.,...Yamamoto, K., 2013, An inter-laboratory evaluation of OD-3 zircon for use as a secondary U–Pb dating standard. Isl. Arc, 22, 382–394.
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