Timescale of material circulation in subduction zone: U–Pb zircon and K–Ar phengite double‐dating of the Sanbagawa metamorphic complex in the Ikeda district, central Shikoku, southwest Japan-Reference-Cited by-同舟云学术

Timescale of material circulation in subduction zone: U–Pb zircon and K–Ar phengite double‐dating of the Sanbagawa metamorphic complex in the Ikeda district, central Shikoku, southwest Japan

Published:2019-05-07 Issue:4 Volume:28 Page:
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Nagata Mitsuhiro¹²,Miyazaki Kazuhiro²,Iwano Hideki³,Danhara Tohru³,Obayashi Hideyuki⁴,Hirata Takafumi⁵,Yagi Koshi⁶,Kouchi Yoshikazu¹,Yamamoto Koshi⁷,Otoh Shigeru¹

Affiliation:

1. Department of New Energy Science, Graduate School of Science and EngineeringUniversity of Toyama 3190 Gofuku, Toyama 930‐8555 Japan

2. Institute of Geology and Geoinformation, Geological Survey of JapanAdvanced Industrial Science and Technology (AIST) Central 7, 1‐1‐1 Higashi, Tsukuba Ibaraki 305‐8567 Japan

3. Kyoto Fission‐Track Co., Ltd. 44‐4 Minamitajiri‐cho, Omiya, Kita‐ku, Kyoto 603‐8832 Japan

4. Department of Geology and MineralogyKyoto University Kitashirakawa Oiwakecho, Sakyo‐ku, Kyoto 606‐8502 Japan

5. Geochemical Research CenterThe University of Tokyo 7‐3‐1 Hongo, Bunkyo‐ku, Tokyo 113‐0033 Japan

6. Hiruzen Institute for Geology and Chronology 2‐5 Nakashima, Naka‐ku, Okayama 703‐8252 Japan

7. Department of Earth and Planetary Sciences, Graduate School of Environmental StudiesNagoya University, Furo‐cho, Chikusa‐ku Nagoya Aichi 464‐8601 Japan

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12306

Reference80 articles.

1. Influence of dissolution/reprecipitation reactions on metamorphic greenschist to amphibolite facies mica40Ar/39Ar ages in the Longmen Shan (eastern Tibet)

2. Tectonic boundary between the Sanbagawa belt and the Shimanto belt in central Shikoku, Japan

3. The youngest blueschist belt in SW Japan: implication for the exhumation of the Cretaceous Sanbagawa high-P/T metamorphic belt

4. Recognition of the Shimanto HP metamorphic belt within the traditional Sanbagawa HP metamorphic belt: New perspectives of the Cretaceous–Paleogene tectonics in Japan

5. Existence of New Independent Regional Metamorphic Belt in the Sanbagawa Metamorphic Belt: Orogenic Evolution of Japan from Cretaceous to Tertiary

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