西准噶尔别鲁阿嘎希花岗闪长岩年代学、地球化学特征及岩石成因

杨钢; 肖龙; 王国灿; 高睿; 贺新星; 张雷; 周佩

doi:10.3799/dqkx.2015.066

Volume 40 Issue 5

May 2015

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Yang Gang, Xiao Long, Wang Guocan, Gao Rui, He Xinxing, Zhang Lei, Zhou Pei, 2015. Geochronological, Geochemical and Petrogenesis of Bieluagaxi Granodioritic Pluton in Western Junggar. Earth Science, 40(5): 810-823. doi: 10.3799/dqkx.2015.066

Citation:

Yang Gang, Xiao Long, Wang Guocan, Gao Rui, He Xinxing, Zhang Lei, Zhou Pei, 2015. Geochronological, Geochemical and Petrogenesis of Bieluagaxi Granodioritic Pluton in Western Junggar. Earth Science, 40(5): 810-823. doi: 10.3799/dqkx.2015.066

Citation:

Yang Gang, Xiao Long, Wang Guocan, Gao Rui, He Xinxing, Zhang Lei, Zhou Pei, 2015. Geochronological, Geochemical and Petrogenesis of Bieluagaxi Granodioritic Pluton in Western Junggar. Earth Science, 40(5): 810-823. doi: 10.3799/dqkx.2015.066

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Geochronological, Geochemical and Petrogenesis of Bieluagaxi Granodioritic Pluton in Western Junggar

doi: 10.3799/dqkx.2015.066

Yang Gang^{1, 2
,},
Xiao Long^{2
,
,},
Wang Guocan^{2, 3},
Gao Rui^{2, 4},
He Xinxing^{2, 5},
Zhang Lei^{2, 6},
Zhou Pei²

1.
Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
4.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
5.
Geological Survey of Jiangsu Province, Nanjing 210018, China
6.
Hubei Geological & Mining Exploration Co., Ltd., Wuhan 430022, China

Received Date: 2014-09-20
Publish Date: 2015-05-15

Abstract

Abstract

For a better understanding of the petrogenesis and tectonic environment of the acidic intrusive rocks in Western Junggar, a study is carried out on Bieluagaxi granodioritic pluton located in the Central part of West Junggar. Its petrogenesis, magma source, tectonics setting based on petrography, zircon LA-ICP-MS U-Pb ages, whole-rock major and trace elements, and Sr-Nd isotopic compositions are discussed in detail. LA-ICP-MS U-Pb zircon data of the granodiorite give weighted ages of 318.7±3.3 Ma. Bieluagaxi granodiorite is calc-alkaline suite with high MgO(Mg^#=49-59), Ni and Cr contents. Bieluagaxi granodiorite is strongly enriched in large ion lithophile elements (LILEs, e.g. K, Rb, Sr and Ba), but it displays depletion of high field strength elements (HFSEs, e.g. Nb, Ta and Ti). In terms of Sr-Nd isotopic compositions, granodiorite has low initial ⁸⁷Sr/⁸⁶Sr ratios (0.704 297-0.704 399) and high positive ε_Nd(t) (5.8-6.5). Therefore, we suggest that the early Late Carboniferous Bieluagaxi granodioritic pluton has been generated in a subduction setting, the mantle wedge began to partially melt due to the upward fluid from the dehydration of subducting oceanic slab, resulting in the asthenospheric mafic magma underplating the lower crust. Then, the lower juvenile basaltic crust derived from the depleted mantle underwent partial melting to generate the I type granites of the Bieluagaxi granodioritic pluton.
- Bieluagaxi granodioritic pluton,
- geochronology,
- geochemistry,
- Sr-Nd isotope,
- western Junggar,
- stratigraphy

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References(83)

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Geochronological, Geochemical and Petrogenesis of Bieluagaxi Granodioritic Pluton in Western Junggar

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