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Volume 29 Issue 5
Oct 2018
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Journal of Earth Science  > 2018  >  29(5): 1074-1080.
Jingbo Liu, Neng-Song Chen, Wen Su. Tectonic Boundary and Ceasing Time of Amalgamation be-tween the North China Craton and the North Qinling Belt. Journal of Earth Science, 2018, 29(5): 1074-1080. doi: 10.1007/s12583-018-0847-8
Citation: Jingbo Liu, Neng-Song Chen, Wen Su. Tectonic Boundary and Ceasing Time of Amalgamation be-tween the North China Craton and the North Qinling Belt. Journal of Earth Science, 2018, 29(5): 1074-1080. doi: 10.1007/s12583-018-0847-8
shu

Tectonic Boundary and Ceasing Time of Amalgamation be-tween the North China Craton and the North Qinling Belt

doi: 10.1007/s12583-018-0847-8
  • 1.

    State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

  • 2.

    College of Earth and Planetary Sciences, University of the Chinese Academy of Sciences, Beijing 100049, China

  • 3.

    School of Earth Sciences, Center for Global Tectonics, China University of Geosciences, Wuhan 430074, China

More Information
  • Corresponding author: Jingbo Liu
  • Received Date: 26 May 2018
  • Accepted Date: 27 Jun 2018
  • Publish Date: 01 Oct 2018
    Abstract
  • The Qinling orogenic belt is a composite orogen, consisting of the north and south Qinling belts with different collision ages. The North Qinling belt is composed of several petro-tectonic units, including the Kuanping, Erlangping, Qinling and Danfeng groups with numerous granitoid plutons from Neoproterzoic to Middle Devonian. To the north of the Kuanping Group, a mylonitized granite body in the Luanchuan Group was determined to have the magmatic age of 850 Ma, which is the northernmost Neoprotozoic granite body. The volcanic rocks of the Dahongkou Formation from the Luanchuan Group had the eruptive age of~1 600 Ma, obtained from zircon U-Pb LA-ICP-MS analysis. The detrital zircons in meta-sandstones from the Taowan Group have three populations of~920-1 400, ~1 600-2 100, and >2 200 Ma ages, whereas those from the Kuanping Group shows six populations with the peaks of~590, ~767, ~952, ~1 590, ~2 485, and~3 200 Ma. These data suggest that the boundary between the North China Craton and the North Qinling belt cannot simply be constrained by using the events determined from zircon U-Pb ages. The granitoid plutons with the magmatic age of 430 Ma were strongly deformed, while those with the magmatic age of~390 Ma show no or less deformation, indicating that the deformation of amalgamation between the North China Craton and the North Qinling belt ceased between 390 and 430 Ma.

     

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    • References(22)
  • Cao, H. H., Li, S. Z., Zhao, S. J., et al., 2016. Detrital Zircon Geochronology of Neoproterozoic to Early Paleozoic Sedimentary Rocks in the North Qinling Orogenic Belt:Implications for the Tectonic Evolution of the Kuanping Ocean. Precambrian Research, 279:1-16. https://doi.org/10.1016/j.precamres.2016.04.001
    Chen, D. L., Ren, Y. F., Gong, X. G., et al., 2015. Identification and Its Geological Significance of Eclogite in Songshugou, the North Qinling. Acta Petrologica Sinica, 31(7):1841-1854 (in Chinese with English Abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98201507003
    Cheng, H., Zhang, C., Vervoort, J. D., et al., 2011. Geochronology of the Transition of Eclogite to Amphibolite Facies Metamorphism in the North Qinling Orogen of Central China. Lithos, 125(3/4):969-983. https://doi.org/10.1016/j.lithos.2011.05.010
    Cheng, H., Zhang, C., Vervoort, J. D., et al., 2012. Timing of Eclogite Facies Metamorphism in the North Qinling by U-Pb and Lu-Hf Geochronology. Lithos, 136-139:46-59. https://doi.org/10.1016/j.lithos.2011.06.003
    Diwu, C. R., Sun, Y., Liu, L. A., et al., 2010. The Disintegration of Kuanping Group in North Qinling Orogenic Belts and Neo-Proterozoic N-MORB. Acta Petrologica Sinica, 26:2025-2038 (in Chinese with English Abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201007006
    Diwu, C. R., Sun, Y., Zhang, H., et al., 2012. Episodic Tectonothermal Events of the Western North China Craton and North Qinling Orogenic Belt in Central China:Constraints from Detrital Zircon U-Pb Ages. Journal of Asian Earth Sciences, 47:107-122. https://doi.org/10.1016/j.jseaes.2011.07.012
    Dong, Y. P., Zhang, G. W., Neubauer, F., et al., 2011. Tectonic Evolution of the Qinling Orogen, China:Review and Synthesis. Journal of Asian Earth Sciences, 41(3):213-237. https://doi.org/10.1016/j.jseaes.2011.03.002
    Dong, Y. P., Yang, Z., Liu, X. M., et al., 2014. Neoproterozoic Amalgamation of the Northern Qinling Terrain to the North China Craton:Constraints from Geochronology and Geochemistry of the Kuanping Ophiolite. Precambrian Research, 255:77-95. https://doi.org/10.1016/j.precamres.2014.09.008
    Gong, X. K., Chen, D. L., Ren, Y. F., et al., 2016. Identification of Coesite-Bearing Amphibolite in the North Qinling and Its Geological Significance. Chinese Science Bulletin, 61(12):1365-1378 (in Chinese)
    Henan Institute of Geological Survey, 2001. 1: 250 000 Geological Map of Pingdingshan. Henan Institute of Geological Survey, Zhengzhou (in Chinese)
    Lu, S. N., Li, H. K., Chen, Z. H., et al., 2003. Meso-Neoproterozoic Geological Evolution of the Qinling and Its Respondence to Rodinia Event. Geological Publishing House, Beijing. 1-194 (in Chinese)
    Lu, S. N., Zhao, G. C., Wang, H. C., et al., 2008. Precambrian Metamorphic Basement and Sedimentary Cover of the North China Craton:A Review. Precambrian Research, 160(1/2):77-93. https://doi.org/10.1016/j.precamres.2007.04.017
    Mattauer, M., Matte, P., Malavieille, J., et al., 1985. Tectonics of the Qinling Belt:Build-up and Evolution of Eastern Asia. Nature, 317(6037):496-500. https://doi.org/10.1038/317496a0
    Meng, Q. R., Zhang, G. W., 2000. Geologic Framework and Tectonic Evolution of the Qinling Orogen, Central China. Tectonophysics, 323(3/4):183-196. https://doi.org/10.1016/s0040-1951(00)00106-2
    Shi, Y., Yu, J. H., Santosh, M., 2013. Tectonic Evolution of the Qinling Orogenic Belt, Central China:New Evidence from Geochemical, Zircon U-Pb Geochronology and Hf Isotopes. Precambrian Research, 231:19-60. https://doi.org/10.1016/j.precamres.2013.03.001
    Wang, H., Wu, Y. B., Gao, S., et al., 2011. Eclogite Origin and Timings in the North Qinling Terrane, and Their Bearing on the Amalgamation of the South and North China Blocks. Journal of Metamorphic Geology, 29(9):1019-1031. https://doi.org/10.1111/j.1525-1314.2011.00955.x
    Wang, X. X., Wang, T., Zhang, C. L., 2013. Neoproterozoic, Paleozoic, and Mesozoic Granitoid Magmatism in the Qinling Orogen, China:Constraints on Orogenic Process. Journal of Asian Earth Sciences, 72:129-151. https://doi.org/10.1016/j.jseaes.2012.11.037
    Wang, X. L., Jiang, S. Y., Dai, B. Z., et al., 2011. Age, Geochemistry and Tectonic Setting of the Neoproterozoic (ca. 830 Ma) Gabbros on the Southern Margin of the North China Craton. Precambrian Research, 190(1/2/3/4):35-47. https://doi.org/10.1016/j.precamres.2011.08.004
    Yang, J. S., Xu, Z. Q., Dobrzhinetskaya, L. F., et al., 2003. Discovery of Metamorphic Diamonds in Central China:An Indication of a >4 000-km-Long Zone of Deep Subduction Resulting from Multiple Continental Collisions. Terra Nova, 15(6):370-379. https://doi.org/10.1046/j.1365-3121.2003.00511.x
    Yuan, H. L., Gao, S., Dai, M. N., et al., 2008. Simultaneous Determinations of U-Pb Age, Hf Isotopes and Trace Element Compositions of Zircon by Excimer Laser-Ablation Quadrupole and Multiple-Collector ICP-MS. Chemical Geology, 247(1/2):100-118. https://doi.org/10.1016/j.chemgeo.2007.10.003
    Zhang, G. W., Meng, Q. G., Yu, Z. P., et al., 1996. Orogenesis and Dynamics of the Qinling Orogen. Science in China Series D:Earth Sciences, 39:225-234 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600264788
    Zhao, G. C., Cawood, P. A., 2012. Precambrian Geology of China. Precambrian Research, 222/223:13-54. https://doi.org/10.1016/j.precamres.2012.09.017
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