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Coupling of Jiamusi Uplifting and Surrounding Mesozoic-Cenozoic Basins in Northeast China

LIU Zhi-hong1, ZHOU Fei1, WU Xiang-mei2, SUN Xiao-meng1, ZHAO Cheng-xiang3, MEI Mei1, HUANG Chao-yi1   

  1. 1.College of Earth Sciences, Jilin University, Changchun130061, China;
    2.Research Institute of Exploration and Development, Daqing Oil Field Company, Ltd.| PetroChina, Daqing163712, Heilongjiang, China;
    3.Qinghai Institute of Geological Survey, Xining810001, China
  • Received:2011-05-05 Online:2011-09-26 Published:2011-09-26

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Abstract:

On the basis of the field investigation and geological interpretation of seismic profiles of Jiamusi uplift and surrounding Mesozoic-Cenozoic basins in Northeast China, combined with recent research results, the basin-mountain coupling are determined: the study area occurred NW-SE extension, formed NE trending extensional basin-mountain coupling system in the Early Cretaceous; suffered NWW-SEE compression, formed the NE-NNE trending compressive basin-mountain coupling system which consists of thrust and compressive basin in the Late Cretaceous; experienced nearly NS trending compression, not only the Cretaceous formation of NE-NNE trending structures and basins were superimposed, but also formed the nearly EW trending compressive basinmountain coupling system which consists of uplifts and compressive depression basins in OligoceneMiocene. The uplifting of Jiamusi uplift in Mesozoic-Cenozoic is mainly the results of twice thrusting superposition in Late Cretaceous and Oligocene-Miocene. The study area has always been active continental margin tectonic setting since the Cretaceous, the above three stages of basin-mountain coupling are related with the subduction of the Pacific plate to the Eurasian plate.

Key words: structural feature, Mesozoic-Cenozoic basins, basin-range coupling, Jiamusi uplift, deformation time;tectonics

CLC Number: 

  • P542.4
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