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  1. B100 理学部/理学研究科
  2. B100b 刊行物
  3. The Journal of earth and planetary sciences
  4. 57

CHIME geochronology of granitic gneiss from Baekdong in the Hongseong area of the Gyeonggi Massif, South Korea

https://doi.org/10.18999/joueps.57.19
https://doi.org/10.18999/joueps.57.19
6e2b92f7-3ab0-43d4-96f8-50ecd9f516a8
名前 / ファイル ライセンス アクション
57-2.pdf 57-2.pdf (3.8 MB)
アイテムタイプ 紀要論文 / Departmental Bulletin Paper(1)
公開日 2011-05-06
タイトル
タイトル CHIME geochronology of granitic gneiss from Baekdong in the Hongseong area of the Gyeonggi Massif, South Korea
言語 en
著者 SUZUKI, Kazuhiro

× SUZUKI, Kazuhiro

WEKO 40470

en SUZUKI, Kazuhiro

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CHWAE, Ueechan

× CHWAE, Ueechan

WEKO 40471

en CHWAE, Ueechan

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DUNKLEY, Daniel J.

× DUNKLEY, Daniel J.

WEKO 40472

en DUNKLEY, Daniel J.

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KIM, Sung-Won

× KIM, Sung-Won

WEKO 40473

en KIM, Sung-Won

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KAJIZUKA, Izumi

× KAJIZUKA, Izumi

WEKO 40474

en KAJIZUKA, Izumi

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MINAMI, Masayo

× MINAMI, Masayo

WEKO 40475

en MINAMI, Masayo

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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
抄録
内容記述タイプ Abstract
内容記述 CHIME dating was carried out on zircon and allanite in a sample of granitic gneiss from the Deokjeongri Granitic Gneiss, exposed at Baekdong (36°33.521'N, 126°44.131'E) in the Hongseong area, which lies in the southwestern Palt of the Gyeonggi Massif. Geochemically, the sample belongs to the high-K(calc-alkaline series or shoshonite series of A-type granites, and is typical of within-plate granitoids. The CHIME ages for concentrically-zoned zircon cores and the core of an exceptionally large allanite grain are 824±29 Ma and 825±110 Ma, respectively. Outer growth zones in zircon with low Y2O3 and margins with high Y2O3 yield poorly defined ages of ca. 500 Ma and 230 Ma, respectively. Allanite rims give ages which cluster along two isochrons, 438±99 Ma for low-Y2O3 domains in equilibrium with Ca-rich garnet, and 254±30 Ma for high Y2O3 domains that formed during the breakdown of garnet. The present sample differs from granitic gneisses in the same lithological unit from other sites, in terms of both ages and geochemistry. Such diversity suggests that the Deokjeongri Granitic Gneiss is a composite unit, comprised of a variety of protoliths from differing tectonic environments and with differing tectonometamorphic histories.
言語 en
出版者
出版者 Dept. of Earth and Planetary Sciences, Nagoya University
言語 en
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.57.19
ID登録タイプ JaLC
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 57, p. 19-41, 発行日 2010
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/14733
識別子タイプ HDL
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