Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (3): 781-797.doi: 10.13278/j.cnki.jjuese.201603114

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Discussion on the Relationship Between Pan Pacific Plate Movement and Mesozoic Geological Evolution of Eastern Chinese Continent

Yang Haibin1,2, Tian Xiaobo1, Bai Zhiming1, Zhang Zhongjie1   

  1. 1. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;
    2. College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China
  • Received:2015-11-14 Online:2016-05-26 Published:2016-05-26
  • Supported by:

    Supported by National Natural Science Foundation (41274066) and Projects of State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, CAS

Abstract:

This paper aims to reveal the relationships between the temperal-spatial distribution of geological recordings, like magmatism, structure and sedimentary basin, and the movement of Pan Pacific plate which intensively influenced the Eastern Chinese continent. As a consequence, variation of plate subducting angle, velocity and direction can produce a great impact on the continent overlying. The Eastern Chinese continent, consisting of Northeast China (NEC), North China(NC) and South China(SC), all were influenced by the Pan Pacific plate subduction on the eastern borde. Due to their various inherent properties, different plates had experienced different geological evolution. Based on discussion on some phenomena characterized as full of anomalies, some conclusions can be drawn for further test. Firstly, through mechanical analysis of possible triple junctions ever existing in eastern China continental frontier, it is suggested that the TTT, TTR or TFT modes should work there, rather than the simplified stable passive continental boundary. Secondly, the origin of west-east distribution of magmatism in central SC might call the ridge of Farallon and Izanagi plate as a reference. The NWW-extending ridge expanding of Izanagi and Pacific could result in the backward movement of plate blocks from the Late Jurassic to Early Cretaceous. Thirdly, few evidence supports the subduction ever took place in the eastern NC, which leads to the hypothesis that the Tanlu fault, the inherent weak part of NC, could have performed as other continent margin, which can be indicated by the strong coupling of plate motion and the corresponding activities of Tanlu fault in Jurassic and Early Cretaceous, instead of plate subduction under NC.

Key words: Eastern Chinese continent, Pacific plate, plate subduction, Mesozoic and Cenozoic, Tanlu fault, triple junctions

CLC Number: 

  • P541

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