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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2005  >  27(5): 449-454
Ji Rangshou, Gao Changlin. TECTONIC EVOLUTION AND BASIN FORMATION OF THE MESOZOIC AND CENOZOIC ON THE BOTH SIDES OF QINLING-DABIE OROGENIC BELT[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2005, 27(5): 449-454. doi: 10.11781/sysydz200505449
Citation: Ji Rangshou, Gao Changlin. TECTONIC EVOLUTION AND BASIN FORMATION OF THE MESOZOIC AND CENOZOIC ON THE BOTH SIDES OF QINLING-DABIE OROGENIC BELT[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2005, 27(5): 449-454. doi: 10.11781/sysydz200505449
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TECTONIC EVOLUTION AND BASIN FORMATION OF THE MESOZOIC AND CENOZOIC ON THE BOTH SIDES OF QINLING-DABIE OROGENIC BELT

doi: 10.11781/sysydz200505449

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

  • Received Date: 2004-12-16
  • Rev Recd Date: 2005-07-22
  • Publish Date: 2005-09-25
    Abstract
  • Since the Indosinian epoch,under a condensing tectonic environment compressed from3 sides,the Chinese continent has experienced 4 stages of tectonic evolution:T3—J2,J3—K1,K2—E,and E3/N-Q,resultingin corresponding basin prototypes along both sides of the Qinling-Dabie orogenic belt.The 1ststageis characterised by compressional intracontinental foreland basin prototype,the 2nd by compressionalintracontinental foreland and strike-slip basin prototype,the 3rd by extentional rift-subsidence basin proto-type,and the 4th by down-warped basin prototype.

     

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