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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. 55

CHIME dating of monazite from the Dongqing pluton in SE Jilin, China

https://doi.org/10.18999/joueps.55.23
https://doi.org/10.18999/joueps.55.23
3eccaa82-4ea8-4dc9-b9f6-ef38292c68c1
名前 / ファイル ライセンス アクション
55-2.pdf 55-2.pdf (1.7 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2011-05-06
タイトル
タイトル CHIME dating of monazite from the Dongqing pluton in SE Jilin, China
言語 en
著者 SUN, Deyou

× SUN, Deyou

WEKO 40443

en SUN, Deyou

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SUZUKI, Kazuhiro

× SUZUKI, Kazuhiro

WEKO 40444

en SUZUKI, Kazuhiro

Search repository
KAJIZUKA, Izumi

× KAJIZUKA, Izumi

WEKO 40445

en KAJIZUKA, Izumi

Search repository
KAMIKUB0, Hiroshi

× KAMIKUB0, Hiroshi

WEKO 40446

en KAMIKUB0, Hiroshi

Search repository
Lu, Xiaoping

× Lu, Xiaoping

WEKO 40447

en Lu, Xiaoping

Search repository
Wu, Fuyuan

× Wu, Fuyuan

WEKO 40448

en Wu, Fuyuan

Search repository
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 The Dongqing pluton in the Zhangguangcai Range, NE China comprises two-mica monzogranite and garnet-bearing two-mica monzogranite with subordinate garnetbearing muscovite alkali-feldspar granite. The monzogranite was dated as 208 Ma by the ^208Pb/^232Th monazite dating (Fang, 1992) and ca. 160 Ma by the Rb-Sr and Sm-Nd methods (Wu et al., 2004). To examine the discrepancy, monazite from the monzogranite was dated by the CHIME method coupled with age mapping. Monazite grains show significant compositional variation in concentric and sector fashions, but are chronologically uniform. Individual sets of ThO2, UO2 and PbO analyses were screened by the chemical criteria, 0.96<(Ca+Si)/(Th+U+Pb+S)<1.05 and K2O<0.02 wt.%. The screened data points are arrayed linearly on the PbO vs. Th02* diagram and define an isochron of 159.0±4.8 Ma with an intercept value of 0.0030±0.0017, suggesting that the older isotopic monazite age is possibly resulted from the sizable amounts of initial Pb. Present CHIME monazite dating reinforces that variety of peraluminous rocks in the Dongqing pluton formed at about 160 Ma through the late stage of magmatic differentiation and magma-fluid interaction.
言語 en
内容記述タイプ Abstract
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.55.23
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 55, p. 23-37, 発行日 2008
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/14729
識別子タイプ HDL
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