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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2003  >  25(6): 729-734
CHEN Qiang-lu, QIAN Yi-xiong, MA Hong-qiang, Wang Shu-yi. DIAGENESIS AND POROSITY EVOLUTION OF THE ORDOVICIAN CARBONATE ROCKS IN TAHE OILFIELD, TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(6): 729-734. doi: 10.11781/sysydz200306729
Citation: CHEN Qiang-lu, QIAN Yi-xiong, MA Hong-qiang, Wang Shu-yi. DIAGENESIS AND POROSITY EVOLUTION OF THE ORDOVICIAN CARBONATE ROCKS IN TAHE OILFIELD, TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(6): 729-734. doi: 10.11781/sysydz200306729
shu

DIAGENESIS AND POROSITY EVOLUTION OF THE ORDOVICIAN CARBONATE ROCKS IN TAHE OILFIELD, TARIM BASIN

doi: 10.11781/sysydz200306729
  • 1.

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

  • 2. Western Subdivision of Exploration & Production Research Institute, SINOPEC, Urumqi, Xinjiang 830011,China

  • Received Date: 2003-04-05
  • Rev Recd Date: 2003-10-28
  • Publish Date: 2003-11-25
    Abstract
  • The carbonates of Ordovician are the principal reservoirs in Tahe oilfield,Tarim Basin.The diagenesis of Ordovician carbonates is characterized by multiple stages,different types and enviroments.The major diagenesis includes cementation,solution,fracture and hydrothermal diagenesis which controlled the evolution of reservoirs.The history of dagenesis and porosity evolution and the origin of formation of the Ordovician reservoirs were reconverted.

     

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