An Zuoxiang. NON-MARINE SEDIMENTARY FACIES AND DISTRIBUTION OF SOURCE ROCKS AND RESERVOIRS IN CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(1): 1-7. doi: 10.11781/sysydz199501001
Citation: An Zuoxiang. NON-MARINE SEDIMENTARY FACIES AND DISTRIBUTION OF SOURCE ROCKS AND RESERVOIRS IN CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1995, 17(1): 1-7. doi: 10.11781/sysydz199501001

NON-MARINE SEDIMENTARY FACIES AND DISTRIBUTION OF SOURCE ROCKS AND RESERVOIRS IN CHINA

doi: 10.11781/sysydz199501001
  • Received Date: 1994-09-16
  • Publish Date: 1995-01-25
  • For scores of years,the petroleum exploration of China has been mainly targeted at non-marine sedimentary facies.However,the relations of sedimentary patterns with source and reservoir rocks are roughly as follows:source rocks occurred in deep lacustrine,hypabyssal lacustrine and paludal facies,while reservoir rocks could be developed in various environments,in China being predominated by deltaic facies,alluvial fan and shallow lake beach-bar,as well as the weathering crust of basinal basement rocks.During the process of sedimentation,the source and reservoir rocks generally occurred in cycles,which can be grouped into source-reservoir-cap assemblages distinguished as 4 types i.e.lower,upper,auto-land lateral geneses.

     

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