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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 1995  >  17(1): 8-16
Ji Youliang, Zhao Chenlin, Liu Menghui. THE FLUID-FLOWING CONVECTION AND THE FORMATION OF DIAGENETIC TRAPS IN THE DONGPU DEPRESSION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(1): 8-16. doi: 10.11781/sysydz199501008
Citation: Ji Youliang, Zhao Chenlin, Liu Menghui. THE FLUID-FLOWING CONVECTION AND THE FORMATION OF DIAGENETIC TRAPS IN THE DONGPU DEPRESSION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(1): 8-16. doi: 10.11781/sysydz199501008
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THE FLUID-FLOWING CONVECTION AND THE FORMATION OF DIAGENETIC TRAPS IN THE DONGPU DEPRESSION

doi: 10.11781/sysydz199501008

  • Petroleum University, China

  • Received Date: 1993-01-26
  • Publish Date: 1995-01-25
    Abstract
  • The discussions are made on the influence of fluid-flowing convection over the formation and distribution of secondary pores.It is pointed out that the upwelling of fluid-flowing should cease in the depth of 4000m in the reservoirs of the depression due to the barrier fault of upward dipping players,the existence of overpressure and insufficient fluid source.Therefore,the thermal-cyclic convection flowing is predominated and the continuous transformation of soluted material took place by the convection flowing,bringing about the formation of secondary pores and diagenetic traps in deep part of the Dongpu Depression

     

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    • References(3)
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    沃马克.施密特等著,陈荷立等译.砂岩成岩过程中的次生储集孔隙.北京:石油工业出版社,1979
    [2]
    Surdam RC.Organic-Inorganic Interactions and Sandstone Diagenesis.AAPG BC-LL,1989,73(1)
    [3]
    Wood JR,Hewett TA.Reservoir Diagenesis and Convective Fluid Flow.Clastic Diagenesis Edited by David.A.Mcdon-aId.AAPG Menoir,1984.37
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