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Volume 42 Issue 6
Nov.  2020
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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2020  >  42(6): 972-980
LI Tianyu, JIN Jun, TIAN Ying, ZHU Rong, LIU Yifeng. Chemical characteristics of formation water and the relationship with oil and gas preservation on northwestern margin of Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(6): 972-980. doi: 10.11781/sysydz202006972
Citation: LI Tianyu, JIN Jun, TIAN Ying, ZHU Rong, LIU Yifeng. Chemical characteristics of formation water and the relationship with oil and gas preservation on northwestern margin of Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2020, 42(6): 972-980. doi: 10.11781/sysydz202006972
shu

Chemical characteristics of formation water and the relationship with oil and gas preservation on northwestern margin of Junggar Basin

doi: 10.11781/sysydz202006972
  • 1.

    Ocean College, Zhejiang University, Zhoushan, Zhejiang 316021, China

  • 2.

    Research Institute of Experiment and Testing, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China

  • Received Date: 2020-01-02
  • Rev Recd Date: 2020-10-10
  • Publish Date: 2020-11-28
    Abstract
  • The northwestern margin of the Junggar Basin is rich in oil and gas, and the relationship between oil and water is complicated. A large amount of formation water data was used to examine the vertical and lateral distribution of the water chemistry in oil-bearing strata from the Carboniferous to the Cretaceous. Combined with the geological background, the Hongshanzui Oilfield was dissected and the relationship between the chemical characteristics of formation water and the preservation of oil and gas is discussed. The results show that the formation water salinity decreases gradually when the burial depth varies from deep to shallow layers and the stratigraphic age varies from old to new. From the Carboniferous to the Cretaceous, the high salinity area of the formation water gradually migrates from the northwestern margin to the interior of the basin. The margin of the basin or the Ke-Wu fracture hanging wall is greatly affected by the infiltration and leaching of surface water or atmospheric water. The formation water is in a free alternating circulation zone, with low salinity, low chloride ion concentration Na2SO4 type or NaHCO3 type water. The formation is poorly sealed, and heavy oil is usually formed. To the interior of the basin or the Ke-Wu fracture footwall, the formation water is in an alternating or stable stagnation zone, with a high degree of concentration. There mainly exists high salinity and high chloride ion concentration CaCl2 type water. The formation has good sealing properties and forms well-preserved medium-light oil.

     

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