Paleoproterozoic to Cenozoic zircon U–Pb ages with Hf signatures from metamorphic rocks and granodiorite of Tokunoshima: constraints on the geotectonic subdivision of the Ryukyu island arc, Southwest Japan-Reference-Cited by-同舟云学术

Paleoproterozoic to Cenozoic zircon U–Pb ages with Hf signatures from metamorphic rocks and granodiorite of Tokunoshima: constraints on the geotectonic subdivision of the Ryukyu island arc, Southwest Japan

Published:2020-12-27 Issue:3 Volume:64 Page:425-440
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Yamamoto Hiroshi¹^ORCID,Okamoto Kazuaki²,Chung Sun-Lin³⁴,Lee Hao-Yang³,Mita Yuji²,Ueda Shuro¹,Terabayashi Masaru⁵

Affiliation:

1. Graduate School of Science and Engineering, Kagoshima University, Kagoshima, Japan

2. Department of Earth Sciences, Faculty of Education, Saitama University, Saitama, Japan

3. Academia Sinica, Institute of Earth Sciences, Taipei, Taiwan

4. Department of Geosciences, National Taiwan University, Taipei, Taiwan

5. Faculty of Engineering and Design, Kagawa University, Takamatsu, Japan

Funder

JSPS Grant-in-Aid for Scientific Research

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2020.1858356

Reference88 articles.

1. Early-middle archaean crustal evolution deduced from Lu-Hf and U-Pb isotopic studies of single zircon grains

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3. Provenance diversification within an arc-trench system induced by batholith development: the Cretaceous Japan case

4. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system

5. Reconstructing South China in Phanerozoic and Precambrian supercontinents

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