Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (4): 1005-1025.doi: 10.13278/j.cnki.jjuese.201604103

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Global Early Paleozoic Orogens (Ⅲ): Intracontinental Orogen in South China

Li Sanzhong1,2,3, Li Xiyao1,2, Zhao Shujuan1,2, Yang Zhao1,2, Liu Xin1,2, Guo Lingli1,2, Wang Yongming1,2, Hao Yi4, Zhang Jian1,2, Hu Mengying1,2   

  1. 1. College of Marine Geosciences, Ocean University of China, Qingdao 266100, Shandong, China;
    2. Key Lab of Submarine Geosciences and Prospecting Technique, Ministry of Education, Qingdao 266100, Shandong, China;
    3. Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, Shandong, China;
    4. The First Prospecting Team of Shandong Coal Geology Bureau, Tengzhou 277500, Shandong, China
  • Received:2016-03-16 Online:2016-07-26 Published:2016-07-26
  • Supported by:

    Supported by Key Project of NSFC (Grants 41190072, 41190070, U1606401); NSFC for Distinguished Young Scientists (41325009); Taishan Scholor Program and Aoshan Elite Scientist Plan to Prof. Sanzhong Li

Abstract:

This paper takes South China Early Paleozoic Caledonian intracontinental orogenic belt as an example, analyzing the intracontinental orogenic deformation, magmatic and sedimentary characteristics, the distribution of angular unconformity, fold-thrust belts, and subduction polarity. It was found that E-W-striking Cambrian fold asymmetry and spatial distribution of angular unconformities propagated and became younging towards the north in the Daming Mountain and the Dayaoshan area, indicating that the younging and propagation of north-directed thrusting may resulted from the seuqantially southward collision of the Yunkai block and the Diangui-North Vietanam blocks. Under the global tectonic setting, the deformation may be related to far-field intracontinental effect caused by sequential collision of some blocks in the South China block to the northern margin of Gondwana. The Yuanbaoshan and Yuechengling area in the north Guangxi, and the Hunan-Jiangxi border area developed the Early Paleozoic NE-NNE-trending folds and thrusts of which asymmetry indicates westward propagation, probably resulting from the collision of the Cathaysia block to the Yangtze block along the Chenzhou-Linwu fault in the Late Ordovician and Early Silurian. In the global view, it may be related to the clockwise rotation and comprehensive collision of the South China block to Gondwana. In summary, the Caledonian tectonic movement as a whole was sequentially propagated from south to north, and from east to west, their deformation intensity is from strong to weak toward the north or the west, reflecting that South China intracontinental collisional orogenic event is a far-field effect of its collision to the Gondwana. During about 450-420 Ma the South China block has been a part of the northern margin of Gondwana.

Key words: intracontinental orogen, Early Paleozoic, nappe-thrust, Cathaysia block, Yangtze block

CLC Number: 

  • P54

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