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  1. B100 理学部/理学研究科
  2. B100b 紀要
  3. The Journal of earth and planetary sciences
  4. 54

Reexamination of CHIME monazite ages for granite samples from Wugongshan and Huangshan, southeastern China

https://doi.org/10.18999/joueps.54.1
https://doi.org/10.18999/joueps.54.1
69a32100-7515-48da-bea6-61379142547b
名前 / ファイル ライセンス アクション
KJ00005455605.pdf KJ00005455605.pdf (912.7 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-03-08
タイトル
タイトル Reexamination of CHIME monazite ages for granite samples from Wugongshan and Huangshan, southeastern China
言語 en
著者 SUZUKI, Kazuhiro

× SUZUKI, Kazuhiro

WEKO 33358

en SUZUKI, Kazuhiro

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KAJIZUKA, Izumi

× KAJIZUKA, Izumi

WEKO 33359

en KAJIZUKA, Izumi

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WANG, Dezi

× WANG, Dezi

WEKO 33360

en WANG, Dezi

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SUWA, Kanenori

× SUWA, Kanenori

WEKO 33361

en SUWA, Kanenori

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利
言語 en
権利情報 Department of Earth and Planetary Sciences,Graduate School of Environmental Studies Nagoya University
権利
言語 ja
権利情報 本文データは学協会の許諾に基づきCiNiiから複製したものである
抄録
内容記述 The ages of granite samples from Wugongshan and Huangshan, southeastern China were reexamined with the CHIME method coupled with screening of possibly concordant monazite analyses by the chemical criterion that 0.95<(Ca+Si)/(Th+U+Pb+S)<1.05. The age mapping technique reveals that monazite grains in sample Wugongshan-2, K-feldspar porphyritic muscovite-biotite granite, are chronologically zoned with the dominant central domain. The CHIME ages are 159±12 Ma for the central domain and 129±14 Ma for the marginal domain. Sample Wugongshan-3, coarse-grained peraluminous muscovite-biotite granite, gives a 164±19 Ma monazite age. The CHIME monazite ages for samples Huangshan-9 and -10, within-plate type muscovite-bearing biotite granites, are 130±19 and 138±6 Ma, respectively. Previous CHIME monazite ages, 173±10 Ma for Wugongshan samples and 162±10 Ma for Huangshan samples (Suzuki et al., 2000), appear to have resulted from mixing of concordant and discordant datasets and/or datasets for different age domains. The revised CHIME monazite ages provide chronological constraint for the tectonic evolution of southeastern China including the change from a subduction-related compressive environment to an extensional environment.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 国立情報学研究所で電子化したコンテンツを使用している。
言語 ja
内容記述タイプ Other
出版者
言語 en
出版者 Dept. of Earth and Planetary Sciences, Nagoya University
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.18999/joueps.54.1
ID登録タイプ JaLC
DOI
関連タイプ isVersionOf
識別子タイプ URI
関連識別子 http://ci.nii.ac.jp/naid/110007149477/
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 0919-875X
書誌情報 en : The Journal of Earth and Planetary Sciences, Nagoya University

巻 54, p. 1-12, 発行日 2007
フォーマット
application/pdf
著者版フラグ
値 publisher
関係URI
関連名称 http://ci.nii.ac.jp/naid/110007149477/
URI
識別子 http://hdl.handle.net/2237/12872
識別子タイプ HDL
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