Onset Timing of Median Tectonic Line (MTL): Constraints from U–Pb Ages of Detrital Zircons from 3 Distinct Cretaceous Sandstone Units Adjacent to the Low-angle MTL in the Mikawa-Ono/Idaira Area, Central Japan
Author:
Affiliation:
1. Department of Earth Science and Astronomy, The University of Tokyo
2. Faculty of Education, Yamagata University
3. Department of Geology and Paleontology, National Museum of Nature and Science
Publisher
Tokyo Geographical Society
Subject
Materials Chemistry
Link
https://www.jstage.jst.go.jp/article/jgeography/128/3/128_128.391/_pdf
Reference67 articles.
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2. Aoki, K., Isozaki, Y., Kofukuda, D., Sato, T., Yamamoto, A., Maki, K., Sakata, S. and Hirata, T. (2014): Provenance diversification within an arc-trench system induced by the batholith development: The Cretaceous Japan case. Terra Nova, 26, 139-149.
3. Aoki, K., Isozaki, Y., Sakata, S. and Hirata, T. (2015): Mid-Paleozoic arc granitoids in SW Japan with Neoproterozoic xenocrysts from South China: new zircon U–Pb ages by LA-ICPMS. Journal of Asian Earth Sciences, 97, 125-135.
4. Araki, Y. and Kitamura, J. (1968): The Median Tectonic Line in middle-eastern Kii peninsula. Memoir Faculty of Education Mie University, 38, 63-72.
5. Eggins, S.M., Kinsley, L.P.J. and Shelley, J.M.G. (1998): Deposition and element fractionation processes of occurring during atmospheric pressure sampling for analysis by ICP-MS. Applied Surface Science, 129, 278-286.
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