Journal of Earth Science

, Volume 29, Issue 5, pp 1074–1080 | Cite as

Tectonic Boundary and Ceasing Time of Amalgamation between the North China Craton and the North Qinling Belt

  • Jingbo LiuEmail author
  • Neng-Song Chen
  • Wen Su
Metamorphism, Magmatism and Tectonic Evolution of Central China Orogenic Belts


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.

Key Words

Qinling orogenic belt Taowan Group Kuanping Group granitoid zircon age 


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This study was supported by the National Natural Science Foundation of China (No. 41372080). Professor Zhendong You guided the first author to finish his thesis studies on the metamorphism of the Qinling-Dabie orogenic belt, as a master student from 1985 to 1988 and as a PHD student from 1991 to 1994. He is a knowledgeable, gentle and kind teacher. This paper is dedicated to Prof. Zhendong You for his birthday of 90 years old. The final publication is available at Springer via

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References Cited

  1. 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. CrossRefGoogle Scholar
  2. 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)Google Scholar
  3. 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. CrossRefGoogle Scholar
  4. 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. CrossRefGoogle Scholar
  5. 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)Google Scholar
  6. 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. CrossRefGoogle Scholar
  7. 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. CrossRefGoogle Scholar
  8. 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. CrossRefGoogle Scholar
  9. 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)Google Scholar
  10. Henan Institute of Geological Survey, 2001. 1: 250.000 Geological Map of Pingdingshan. Henan Institute of Geological Survey, Zhengzhou (in Chinese)Google Scholar
  11. 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)Google Scholar
  12. 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. CrossRefGoogle Scholar
  13. 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. CrossRefGoogle Scholar
  14. Meng, Q. R., Zhang, G. W., 2000. Geologic Framework and Tectonic Evolution of the Qinling Orogen, Central China. Tectonophysics, 323(3/4): 183–196. CrossRefGoogle Scholar
  15. 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. CrossRefGoogle Scholar
  16. 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. CrossRefGoogle Scholar
  17. 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. CrossRefGoogle Scholar
  18. Wang, X. L., Jiang, S. Y., Dai, B. Z., et al., 2011. Age, Geochemistry and Tectonic Setting of the Neoproterozoic (ca. 8.0Ma) Gabbros on the Southern Margin of the North China Craton. Precambrian Research, 190(1/2/3/4): 35–47. CrossRefGoogle Scholar
  19. 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. CrossRefGoogle Scholar
  20. 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. CrossRefGoogle Scholar
  21. 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: 225–234Google Scholar
  22. Zhao, G. C., Cawood, P. A., 2012. Precambrian Geology of China. Precambrian Research, 222/223: 13–54. CrossRefGoogle Scholar

Copyright information

© China University of Geosciences and Springer-Verlag GmbH Germany, part of Springer Nature 2018

Authors and Affiliations

  1. 1.State Key Laboratory of Lithospheric Evolution, Institute of Geology and GeophysicsChinese Academy of SciencesBeijingChina
  2. 2.College of Earth and Planetary SciencesUniversity of the Chinese Academy of SciencesBeijingChina
  3. 3.School of Earth Sciences, Center for Global TectonicsChina University of GeosciencesWuhanChina

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