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Volume 25 Issue 1
Feb 2014
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Journal of Earth Science  > 2014  >  25(1): 74-86.
Songlin Gong, Nengsong Chen, Hongyan Geng, Min Sun, Lu Zhang, Qinyan Wang. Zircon Hf Isotopes and Geochemistry of the Early Paleoproterozoic High-Sr Low-Y Quartz-Diorite in the Quanji Massif, NW China: Crustal Growth and Tectonic Implications. Journal of Earth Science, 2014, 25(1): 74-86. doi: 10.1007/s12583-014-0401-2
Citation: Songlin Gong, Nengsong Chen, Hongyan Geng, Min Sun, Lu Zhang, Qinyan Wang. Zircon Hf Isotopes and Geochemistry of the Early Paleoproterozoic High-Sr Low-Y Quartz-Diorite in the Quanji Massif, NW China: Crustal Growth and Tectonic Implications. Journal of Earth Science, 2014, 25(1): 74-86. doi: 10.1007/s12583-014-0401-2
shu

Zircon Hf Isotopes and Geochemistry of the Early Paleoproterozoic High-Sr Low-Y Quartz-Diorite in the Quanji Massif, NW China: Crustal Growth and Tectonic Implications

doi: 10.1007/s12583-014-0401-2
  • 1.

    Three Gorges Geological Hazards Research Center, Ministry of Education, China University of Geosciences, Wuhan, 430074, China

  • 2.

    Faculty of Earth Sciences, China University of Geosciences, Wuhan, 430074, China

  • 3.

    Department of Earth Sciences, the University of Hong Kong, Hong Kong, China

More Information
  • Corresponding author: Songlin Gong, gsanly@163.com
  • Received Date: 27 Jan 2013
  • Accepted Date: 28 May 2013
  • Publish Date: 01 Feb 2014
    Abstract
  • The metamorphosed Early Paleoproterozoic granitoids in the Quanji massif, Northwestern China provide constraints for relationship between the Tarim Craton and North China Craton. Among granitoids batholiths, rocks of the Mohe quartz-diorite show typically adakitic geochemical characteristics, with medium K2O/Na2O ratios (0.56–1.17) and high Sr (519–619 ppm) low Y (9.37–20.40 ppm) and Yb (0.97–1.77 ppm) concentrations. The rocks have ɛNd(t) values between +2.4 and +4.4 and depleted mantle Nd model ages of 2.43–2.59 Ga. The magmatic zircons have positive ɛHf(t) values ranging from +0.40 to +7.60 and depleted mantle Hf model ages of 2.43–2.70 Ga, with major peaks at ~2.54 and ~2.65 Ga. The geochemical and Nd-Hf isotopic characteristics indicate that the Mohe quartz-dioritic rocks might be formed by partial melting of high-pressure metamorphosed juvenile crustal rocks in post-orogenic extensional regime in the Early Paleoproterozoic. It suggests that important crustal growth occurred in the Quanji massif and the Tarim Craton at ~2.4 and 2.5–2.7 Ga. The Quanji massif and Tarim Craton might share a similar crustal evolution history with the North China Craton in the Neoarchean.

     

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