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Volume 29 Issue 5
Oct 2018
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Journal of Earth Science  > 2018  >  29(5): 1132-1150.
Jin Ba, Lu Zhang, Chuan He, Neng-Song Chen, Timothy M. Kusky, Qinyan Wang, Yusheng Wan, Xiaoming Liu. Zircon and Monazite Ages Constraints on Devonian Magmatism and Granulite-Facies Metamorphism in the Southern Qaidam Block: Implications for Evolution of Proto-and Paleo-Tethys in East Asia. Journal of Earth Science, 2018, 29(5): 1132-1150. doi: 10.1007/s12583-018-0853-x
Citation: Jin Ba, Lu Zhang, Chuan He, Neng-Song Chen, Timothy M. Kusky, Qinyan Wang, Yusheng Wan, Xiaoming Liu. Zircon and Monazite Ages Constraints on Devonian Magmatism and Granulite-Facies Metamorphism in the Southern Qaidam Block: Implications for Evolution of Proto-and Paleo-Tethys in East Asia. Journal of Earth Science, 2018, 29(5): 1132-1150. doi: 10.1007/s12583-018-0853-x
shu

Zircon and Monazite Ages Constraints on Devonian Magmatism and Granulite-Facies Metamorphism in the Southern Qaidam Block: Implications for Evolution of Proto-and Paleo-Tethys in East Asia

doi: 10.1007/s12583-018-0853-x
  • 1.

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

  • 2.

    College of Earth Science, Chengdu University of Technology, Chengdu 610059, China

  • 3.

    Sichuan Institute of Geological Survey, Chengdu 610081, China

  • 4.

    Center for Global Tectonics, China University of Geosciences, Wuhan 430074, China

  • 5.

    Beijing SHRIMP Center, Beijing 100037, China

  • 6.

    State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China

More Information
  • Corresponding author: Lu Zhang
  • Received Date: 10 Jul 2018
  • Accepted Date: 08 Aug 2018
  • Publish Date: 01 Oct 2018
    Abstract
  • High-temperature magma generation process and granulite-facies metamorphism can provide important information about mantle-crustal interaction and tectonic evolution. The strongly peraluminous monzonite pluton, the Jinshuikou cordierite granite on the southern margin of the Qaidam Block, can provide important information about the mantle-crustal interaction and constraints on tectonic transition from Proto-Tethys to Paleo-Tethys. This pluton develops enclaves of mafic granulite, amphibolite and quartzofeldspathic rocks, and is cut by massive monzonitic leuco-granite veins. Zircon and monazite U-Pb dating for the cordierite granite, the granulite enclaves and a massive monzonitic leuco-granite vein reveal that the cordierite granitic magma was generated from Mesoproterozoic continental crust with protolith derived from a provenance that was composed of >2.8 Ga old recycled crustal materials and recorded a~1.7 Ga magmatic event. The continental crust underwent low-pressure granulite-facies metamorphism at~380 Ma ago, whereas the cordierite granite magmas was generated and emplaced during 380 Ma, followed by intrusion of the massive monzonitic leuco-granite vein at circa 370-330 Ma. These data suggest that after the final closure of Proto-Tethys Ocean spreading along the southern Qaidam Block at~420 Ma, break-off of the subducted slab or delamination of the lower crustal base and upwelling of the asthenospheric mantle beneath the southern Qaidam Block occurred before the Mid-Devonian, and that the initiation of the Paleo-Tethys tectonics might initiate near the end of Early-Carboniferous in the East Kunlun-Qaidam region, East Asia.

     

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