The Ashizuri granite-alkaline gabbro complex in the forearc of a Paleogene accretionary complex, Shikoku, Japan: Constraints on evolution by zircon U-Pb age and trace element composition-Reference-Cited by-同舟云学术

The Ashizuri granite-alkaline gabbro complex in the forearc of a Paleogene accretionary complex, Shikoku, Japan: Constraints on evolution by zircon U-Pb age and trace element composition

Published:2020 Issue:6 Volume:54 Page:411-420
ISSN:0016-7002
Container-title:GEOCHEMICAL JOURNAL
language:en
Short-container-title:Geochem. J.

Author:

Matsumoto Takumi¹,Aoki Kazumasa²,Windley Brian F.³,Aoki Shogo²

Affiliation:

1. Department of Applied Science, Okayama University of Science

2. Center for Fundamental Education, Okayama University of Science

3. Department of Geology, The University of Leicester

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Link

https://www.jstage.jst.go.jp/article/geochemj/54/6/54_2.0611/_pdf

Reference49 articles.

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2. Aoki, S., Aoki, K., Tsujimori, T., Sakata, S. and Tsuchiya, Y. (2020) Oceanic-arc subduction, stagnation, and exhumation: zircon U-Pb geochronology and trace-element geochemistry of the Sanbagawa eclogites in central Shikoku, SW Japan. Lithos 358−359, 105378.

3. Belousova, E. A., Griffin, W. L., O’Reilly, S. Y. and Fisher, N. L. (2002) Igneous zircon: Trace element composition as an indicator of source rock type. Contrib. Mineral. Petrol. 143, 602−622.

4. Bonin, B. (2007) A-type granites and related rocks: Evolution of a concept, problems and prospects. Lithos 97, 1−29.

5. Chappell, B. W. and White, A. J. R. (1974) Two contrasting granite types. Pacific Geology 8, 173−174.

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