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Volume 39 Issue 1
Feb.  2020
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Article Navigation >  CARSOLOGICA SINICA  > 2020  >  39(1): 71-79
ZENG Cheng, CHEN Benchi, LI Zongjie, MA Xuejun, XUE Mingxi. Controlling factors of macroscopic oil-water distribution in fractured-vuggy carbonate reservoirs in west of area 10 in the Tahe oilfield[J]. CARSOLOGICA SINICA, 2020, 39(1): 71-79. doi: 10.11932/karst2020y001
Citation: ZENG Cheng, CHEN Benchi, LI Zongjie, MA Xuejun, XUE Mingxi. Controlling factors of macroscopic oil-water distribution in fractured-vuggy carbonate reservoirs in west of area 10 in the Tahe oilfield[J]. CARSOLOGICA SINICA, 2020, 39(1): 71-79. doi: 10.11932/karst2020y001
shu

Controlling factors of macroscopic oil-water distribution in fractured-vuggy carbonate reservoirs in west of area 10 in the Tahe oilfield

doi: 10.11932/karst2020y001
  • 1.

    State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, CAS, Guiyang, Guizhou 550081, China

  • 2.

    Oil Field Department of Science and Technology Ministry, SINOPEC, Beijing 100728, China

  • 3.

    Petroleum Exploration and Production Research Institute, SINOPEC Northwest Oilfield Company, Urumqi, Xinjiang 830001, China

  • 4.

    SINOPEC Petroleum Exploration and Production Research Institute, Beijing 100728, China

  • Publish Date: 2020-02-25
    Abstract
  • Ordovician carbonate fractured-vuggy reservoirs in the Tahe oilfield have strong heterogeneity and complex oil-water distribution. It is of great significance for controlling water and stabilizing oil production in fractured-vuggy reservoirs to reveal the macroscopic oil-water distribution law at a regional scale (10 km × 10 km). Based on the work of omni-directional and high-precision three-dimensional seismic data processing, inversion and interpretation, this paper comprehensively analyzes the karst paleostructure and the oil-water regime in the process of oilfield development, and discusses the controlling factors of the macro-horizontal distribution pattern of oil-water in carbonate fractured-vuggy reservoirs in the Tahe oilfield. The results show that a relatively homogeneous paleokarst aquifer was formed in the middle Caledonian Episode I karst period. After hydrocarbon was injected into the paleokarst aquifer medium in the early Hercynian period, deep hydrothermal activity in the late Hercynian period sealed and fixed the fracture-cave body, resulting in fracture-cave separation, and established the present macroscopic distribution pattern of oil and water in the reservoirs.

     

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