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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2017  >  39(5): 587-592
Xu Chunhua, Wang Yalin. Depression and apophysis structure type and its controls on deposition in the Jiyang Depression, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(5): 587-592. doi: 10.11781/sysydz201705587
Citation: Xu Chunhua, Wang Yalin. Depression and apophysis structure type and its controls on deposition in the Jiyang Depression, Bohai Bay Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(5): 587-592. doi: 10.11781/sysydz201705587
shu

Depression and apophysis structure type and its controls on deposition in the Jiyang Depression, Bohai Bay Basin

doi: 10.11781/sysydz201705587
  • 1.

    Oil and Gas Exploration Management Center, SINOPEC Shengli Oilfield, Dongying, Shandong 257015, China

  • 2. Research Institute of Petroleum Exploration and Production, SINOPEC Shengli Oilfield, Dongying, Shandong 257001, China

  • Received Date: 2017-02-10
  • Rev Recd Date: 2017-08-07
  • Publish Date: 2017-09-28
    Abstract
  • Glutenite oil deposits in steep slope zone are major hydrocarbon exploration targets in rift basins. Drilling proves that near-source coarse debris sediments were well developed on the downthrown side of EW oriented faults. On the contrary, near-source sediments seldom or even did not develop on the downthrown side of N(N)E oriented faults. The article discussed the coupling relationship between bulge and depression, and came up with two kinds of coupling relationship which are the mountain-upheaval basin-sedimentary type and basin-sedimentary mountain-upheaval type, focusing on this special phenomenon and based on the recovery of the denudation quantity in the bulge area. Provenance area, erosion thickness and passageway development degree determined whether near-source sediments deposited or not based on the studies of the Dabie orogenic belt. The deposition characteristics of the downthrown side of the EW and N(N)E oriented faults were analyzed, indicating that the EW faults are syndepositional ones and the N(N)E faults are right-lateral strike-slip ones influenced by the SN extensive stress during Paleogene. The difference between kinematic properties and activity time is the main cause of sedimentation difference.

     

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