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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2009  >  31(2): 119-127
Xu Xuhui, Huang Zeguang, Gao Changlin, Zhang Yuchang. DIKTYOGENESE AND BASINS IN CHINA CONTINENT DURING THE MESOZOIC-CENOZOIC[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(2): 119-127. doi: 10.11781/sysydz200902119
Citation: Xu Xuhui, Huang Zeguang, Gao Changlin, Zhang Yuchang. DIKTYOGENESE AND BASINS IN CHINA CONTINENT DURING THE MESOZOIC-CENOZOIC[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(2): 119-127. doi: 10.11781/sysydz200902119
shu

DIKTYOGENESE AND BASINS IN CHINA CONTINENT DURING THE MESOZOIC-CENOZOIC

doi: 10.11781/sysydz200902119
  • 1.

    Exploration & Production Research Institute, SINOPEC, Beijing 100083, China

  • 2. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

  • Received Date: 2008-09-02
  • Rev Recd Date: 2009-02-09
  • Publish Date: 2009-04-28
    Abstract
  • The Chinese continent was compressed from three directions after the Indosinian orogeny,with 3 periods of diktyogenese movements.The first diktyogenese period could be divided 2 stages.Due to the closing of the Palaeo-Tethys,the foredeeps which were related to squeeezing were developed in the stage 1(T3—J2)in West China.As a result of the closing of the Nujiang Ocean,the squeezing foredeeps were continuously developed in the stage 2(J3—K1).The fault basins were developed in NE China and the former foredeeps were reformed or small pull apart basins were arranged in rows in South China,owing to Izanagi Plate subduction and collision.

     

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