内蒙古巴林右旗巴彦查干岩体年代学与地球化学:对古亚洲洋闭合时间的限定

杜继宇; 陶楠; 郭建超; 江斌; 杜贯新

doi:10.3799/dqkx.2019.215

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3361-3377

Du Jiyu, Tao Nan, Guo Jianchao, Jiang Bin, Du Guanxin, 2019. Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean. Earth Science, 44(10): 3361-3377. doi: 10.3799/dqkx.2019.215

Citation:

Du Jiyu, Tao Nan, Guo Jianchao, Jiang Bin, Du Guanxin, 2019. Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean. Earth Science, 44(10): 3361-3377. doi: 10.3799/dqkx.2019.215

Citation:

Du Jiyu, Tao Nan, Guo Jianchao, Jiang Bin, Du Guanxin, 2019. Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean. Earth Science, 44(10): 3361-3377. doi: 10.3799/dqkx.2019.215

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Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean

doi: 10.3799/dqkx.2019.215

Du Jiyu^{1,2
,},
Tao Nan^{2
,
,},
Guo Jianchao²,
Jiang Bin²,
Du Guanxin²

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Shenyang Center of Geological Surey, China Geological Survey, Shenyang 110034, China

Received Date: 2019-08-28
Publish Date: 2019-11-11

Abstract

Abstract

It is a highly controversial topic about the closure of the Paleo-Asian Ocean. Based on the geochemistry, zircon U-Pb dating and Lu-Hf isotope studies of Bayanchagan pluton in Balinyouqi, in this paper, it discusses its formation age, petrogenesis and the regional tectonic setting. Bayanchagan pluton is two-mica monzogranites. LA-ICP-MS zircon U-Pb dating indicates the two-mica monzogranite formed in the Middle-Late Triassic(232.0-241.7 Ma). The two-mica monzogranite is high in SiO₂, Al₂O₃ and low in MgO, Fe₂O₃, belonging to strongly peraluminous series(A/CNK=1.10-1.25), enriched in light rare earth elements and large ion lithophile elements, and depleted in heavy rare earth elements and high field strength elements(Nb, Ta), showing that it is S-type granite. Hf isotopic analysis results show ε_Hf(t) values of -1.8 to +4.01, two-stage model ages ranging from 1 006 Ma to 1 380 Ma, respectively, indicating that the primary magma was derived from the partial melting of a thickened crust. Combined with the studies of the ophiolitic melange, magmatic belt and sedimentary environment of Late Paleozoic, collision related granites, and so on, it is suggested that the eastern segment of the Paleo-Asian Ocean closed in the Late Permian-Early Triassic, and was at the period of continental collision during Triassic.
- Balinyouqi area,
- Middle-Late Triassic,
- S-type granite,
- geochronology,
- geochemistry,
- Paleo-Asian Ocean

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References(99)

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Geochronology and Geochemistry of Bayanchagan Pluton in Balinyouqi, Inner Mongolia: Implication for Timing of Closure of Paleo-Asian Ocean

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