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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2004  >  26(3): 219-222
CHEN Yao-kun, LIAO Zong-ting, WEI Zhi-hong, LI Ming-hui. CHARACTERISTICS AND TECTONIC EVOLUTION OF THE LANPING-SIMAO MESOZOIC BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2004, 26(3): 219-222. doi: 10.11781/sysydz200403219
Citation: CHEN Yao-kun, LIAO Zong-ting, WEI Zhi-hong, LI Ming-hui. CHARACTERISTICS AND TECTONIC EVOLUTION OF THE LANPING-SIMAO MESOZOIC BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2004, 26(3): 219-222. doi: 10.11781/sysydz200403219
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CHARACTERISTICS AND TECTONIC EVOLUTION OF THE LANPING-SIMAO MESOZOIC BASIN

doi: 10.11781/sysydz200403219
  • 1.

    School of Ocean and the Earth Sciences, Tongji University, Shanghai 200092, China

  • 2. Southern Petroleum Exploration and Development Division Company, SINOPEC, Kunming, Yunnan 650200, China

  • Received Date: 2002-10-14
  • Rev Recd Date: 2004-04-03
  • Publish Date: 2004-05-25
    Abstract
  • The Lanping-Simao Mesozoic Basin is a sedimentary basin which was developed based on the Paleo-Tethys multi-island ocean framework,and its formation and evolution are closely related to the tectonic evolution of the Tethys-Sanjiang orogenic belt.The prototype basin was formed during the Middle Triassic accompanying the open of the Mid-Tethys Ocean.The closing of the Mid-Tethys made the crust deformed and the Lower Jurassic missed universally during the end of the Late Triassic to the Early Jurassic.The Neo-Tethys opened during the Middle Jurassic.It made the basin subside again and accept the Middle Jurassic-Cretaceous deposit.Himalayan orogenic movement made the Neo-Tethys closed,and the crust uplifted large scale when the basin was deformed to form fractures,folds and characteristic ramp structures.Then the Cenozoic pull-apart basin superposed on the Mesozoic basin.The tectonic evolution controlled the subsidence,sedimentation,pyrogenesis and structure framework of the basin.

     

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