Origin and Geodynamic Implications of Concealed Granite in Shadong Tungsten Deposit, Xinjiang, China: Zircon U-Pb Chronology, Geochemistry, and Sr-Nd-Hf Isotope Constraint

Chao Chen; Xinbiao Lü; Chunming Wu; Xiao Jiang; Chen Mao

doi:10.1007/s12583-017-0808-7

Volume 29 Issue 1

Jan 2018

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Journal of Earth Science > 2018 > 29(1): 114-129.

Chao Chen, Xinbiao Lü, Chunming Wu, Xiao Jiang, Chen Mao. Origin and Geodynamic Implications of Concealed Granite in Shadong Tungsten Deposit, Xinjiang, China: Zircon U-Pb Chronology, Geochemistry, and Sr-Nd-Hf Isotope Constraint. Journal of Earth Science, 2018, 29(1): 114-129. doi: 10.1007/s12583-017-0808-7

Citation:

Chao Chen, Xinbiao Lü, Chunming Wu, Xiao Jiang, Chen Mao. Origin and Geodynamic Implications of Concealed Granite in Shadong Tungsten Deposit, Xinjiang, China: Zircon U-Pb Chronology, Geochemistry, and Sr-Nd-Hf Isotope Constraint. Journal of Earth Science, 2018, 29(1): 114-129. doi: 10.1007/s12583-017-0808-7

Citation:

Chao Chen, Xinbiao Lü, Chunming Wu, Xiao Jiang, Chen Mao. Origin and Geodynamic Implications of Concealed Granite in Shadong Tungsten Deposit, Xinjiang, China: Zircon U-Pb Chronology, Geochemistry, and Sr-Nd-Hf Isotope Constraint. Journal of Earth Science, 2018, 29(1): 114-129. doi: 10.1007/s12583-017-0808-7

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Origin and Geodynamic Implications of Concealed Granite in Shadong Tungsten Deposit, Xinjiang, China: Zircon U-Pb Chronology, Geochemistry, and Sr-Nd-Hf Isotope Constraint

doi: 10.1007/s12583-017-0808-7

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
No. 6 Geological Survey Team, Bureau of Xinjiang Geological Exploration, Hami 839000, China

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Corresponding author: Xinbiao Lü, 748555304@qq.com
Received Date: 11 Jan 2017
Accepted Date: 27 May 2017
Publish Date: 01 Feb 2018

Abstract

Abstract

Shadong deposit is the first large-scale tungsten deposit found in the East Tianshan orogenic belt, and the geologic characteristics of the deposit indicate that the deeply concealed granite body is genetically related with the mineralization. The LA-ICPMS U-Pb age of zircons from the Shadong concealed granite obtained in this research is 239±2.0 Ma, belonging to the Middle Triassic. The whole rock samples are metaluminous to slightly peraluminous (A/CNK=0.95–1.02) with low contents of SiO₂ (64.0 wt.%–68.5 wt.%) and low K₂O/Na₂O ratios (0.73–0.96). The samples reveal enrichment of K, Rb, Th and depletion of Nb, Ta, P, Ti and have a negative slope from La to Lu (La_N/Yb_N=16.29–36.8) with weak negative Eu anomaly (Eu/Eu^*=0.71–0.82). Initial ⁸⁷Sr/⁸⁶Sr ratios of whole rock range of 0.706 59–0.707 75, ε_Nd(t) values range from -1.77 to -2.53 and ε_Hf(t) values of zircon are between 2.54 and 4.90. The lithogeochemistry and Sr-Nd-Hf isotopic characteristics revealed that the concealed granite in Shadong tungsten deposit is Ⅰ-type granite, and occurs in an intraplate tectonic setting. The magma mixing during intraplating of mantle derived magma intruding into the crust in Indosinian Period is the major formation mechanism of the granite. Of which, the proportion of mantle derived magma ranges from 58% to 60%, and the crustal materials are mainly the metamorphic basement of Xingxingxia Group of Mesoproterozoic Changcheng System, which may provide the main source of ore forming metals of Shadong tungsten deposit.
- East Tianshan,
- Shadong tungsten deposit,
- zircon U-Pb chronology,
- lithogeochemistry,
- Sr-Nd-Hf isotope

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References(91)

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