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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2014  >  36(2): 136-143
Tan Xianfeng, Jiang Yanxia, Tian Jingchun, Zou Guoliang, Li Hang, Wang Weiqing. Sequence interface characteristics and spatial and temporal properties of Kongdian Formation of Paleogene in Jiyang Depression[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(2): 136-143. doi: 10.11781/sysydz201402136
Citation: Tan Xianfeng, Jiang Yanxia, Tian Jingchun, Zou Guoliang, Li Hang, Wang Weiqing. Sequence interface characteristics and spatial and temporal properties of Kongdian Formation of Paleogene in Jiyang Depression[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(2): 136-143. doi: 10.11781/sysydz201402136
shu

Sequence interface characteristics and spatial and temporal properties of Kongdian Formation of Paleogene in Jiyang Depression

doi: 10.11781/sysydz201402136
  • 1.

    Chongqing University of Science and Technology, Chongqing 401331, China

  • 2. State Key Laboratory for Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, Sichuan 610059, China

  • 3. Exploration Department of Changqing Oil Field, PetroChina, Xi'an, Shaanxi 710021, China

  • 4. Geologic Research Institute of SINOPEC Shengli Oilfield Company, Dongying, Shandong 257015, China

  • Received Date: 2013-06-20
  • Rev Recd Date: 2014-02-11
  • Publish Date: 2014-03-28
    Abstract
  • Based on seismic, logging, drilling cores and geochemical data, the sequence boundaries of the Kongdian Formation of Paleogene in the Jiyang Depression were systematically studied. On seismic profiles, the boundaries were featured by onlap, downlap, truncation, toplap and concordance. The drilling cores showed weathering crust and lithology-lithofacies transformation characteristics. The rock-electricity relation indicated different types of mutations. The trace elements also showed mutation characteristics. Four sequence boundaries were identified, including the 1st-order sequence interface TSB1, the 2nd-order sequence interface SSB1 and the 3rd-order sequence interfaces SB1 and SB2. As regional unconformity, the sequence interface TSB1 reflected basin transformation. The sequence interface SSB1 was constructed ceremony conversion surface and showed basin rift stage. The sequence interfaces SB1 and SB2 were climate transformation surfaces and showed the cyclic changes in climate factors. The sequence boundaries were significant for the studies of basin formation, climate change and screen fracture activity.

     

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