Origin of the Hida Belt, Central Japan, with Respect to the Late Triassic Granitoids-bearing Cretaceous Provenance: U–Pb Dating and Trace Element Geochemistry of Detrital Zircons in Tetori Sandstones-Reference-Cited by-同舟云学术

Origin of the Hida Belt, Central Japan, with Respect to the Late Triassic Granitoids-bearing Cretaceous Provenance: U–Pb Dating and Trace Element Geochemistry of Detrital Zircons in Tetori Sandstones

Published:2024-06-25 Issue:3 Volume:133 Page:195-218
ISSN:0022-135X
Container-title:Journal of Geography (Chigaku Zasshi)
language:en
Short-container-title:J. Geogr.

Author:

ISOZAKI Yukio¹^ORCID,IWANO Hideki²³^ORCID,SAWAKI Yusuke¹^ORCID,KUNUGIZA Keitaro⁴^ORCID,HIRATA Takafumi³^ORCID

Affiliation:

1. Department of Earth Science and Astronomy, The University of Tokyo

2. Kyoto Fission-Track Co. Ltd.

3. Geochemical Research Center, The University of Tokyo

4. Toyama Center, Open University of Japan

Publisher

Tokyo Geographical Society

Link

https://www.jstage.jst.go.jp/article/jgeography/133/3/133_133.195/_pdf

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5. Coutts, D.S., William, A.M. and Hubbard, S.M. (2019): Assessment of widely used methods to derive depositional ages from detrital zircon populations. Geoscience Frontiers, 10, 1421-1435.