WANG Ju-feng, CAI Xi-yuan, DENG Hong-wen, SU Fa-qing. EVOLUTION OF BASE-LEVEL CYCLES AND LITHOLOGIC TRAPS OF THE SHA-3 MEMBER IN THE CENTRAL SAG OF THE DONGYING DEPRESSION, THE BOHAIWAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(4): 357-361. doi: 10.11781/sysydz200304357
Citation: WANG Ju-feng, CAI Xi-yuan, DENG Hong-wen, SU Fa-qing. EVOLUTION OF BASE-LEVEL CYCLES AND LITHOLOGIC TRAPS OF THE SHA-3 MEMBER IN THE CENTRAL SAG OF THE DONGYING DEPRESSION, THE BOHAIWAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(4): 357-361. doi: 10.11781/sysydz200304357

EVOLUTION OF BASE-LEVEL CYCLES AND LITHOLOGIC TRAPS OF THE SHA-3 MEMBER IN THE CENTRAL SAG OF THE DONGYING DEPRESSION, THE BOHAIWAN BASIN

doi: 10.11781/sysydz200304357
  • Received Date: 2003-03-11
  • Rev Recd Date: 2003-06-04
  • Publish Date: 2003-07-25
  • Based on study of drilling data and seismic data, the high-resolution sequence stratigraphical framework of Sha-3 member in the central sag of Dongying depression has been established. The middle member of Sha-3 can be divided into one long-term and six short-term of base level cycles. In accordance with the characteristics of the base levels and the forming mechanism of the sandbody, the lithologic traps can be divided into three types: slump turbidite trap, slope-moving turbidity fan trap and sublacustrine fan trap. The formation of traps was related to the evolution of base levels. The sub-lacustrine fan and slope-moving turbidity fan which consisted of the main reservoirs were formed during rising stage of the base level, and the slump turbidite was formed during the falling of base level.

     

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