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Volume 38 Issue 3
Jun.  2019
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Article Navigation >  CARSOLOGICA SINICA  > 2019  >  38(3): 427-437
LIANG Chengpeng, DAN Yong, XU Shenglin, LI Fuxiang, PANG Chunyu, WEI Jiaqi. Interlayer karst reservoir characteristics and development controlling factors of Ordovician in the Xinken area，Tarim basin[J]. CARSOLOGICA SINICA, 2019, 38(3): 427-437. doi: 10.11932/karst20190301
Citation: LIANG Chengpeng, DAN Yong, XU Shenglin, LI Fuxiang, PANG Chunyu, WEI Jiaqi. Interlayer karst reservoir characteristics and development controlling factors of Ordovician in the Xinken area，Tarim basin[J]. CARSOLOGICA SINICA, 2019, 38(3): 427-437. doi: 10.11932/karst20190301
shu

Interlayer karst reservoir characteristics and development controlling factors of Ordovician in the Xinken area，Tarim basin

doi: 10.11932/karst20190301
  • 1.

    Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu,Sichuan 610059,China

  • 2.

    Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu,Sichuan 610059,China/Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics,MNR & GZAR, Guilin, Guangxi 541004, China

  • Publish Date: 2019-06-25
    Abstract
  • The fracture zone of the Ordovician system interlayer karst area in the Xinken area of of Tarim basin is a favorable area for oil and gas exploration in the north of Tarim basin in recent years. Analysis suggests that the reservoirs in this area are dominated by fracture-hole and karst reservoirs, and mainly in the longitudinal direction of 100 m below the top surface of the Yijianfang formation. Based on sedimentary environment, paleogeomorphology reconstruction and karst conditions, it is considered that the relatively pure limestone deposited on the platform facies is the foundation of karst. The karst exposure period of Yijianfang formation formed early small pores, while during the Lianglitage exposure period, underground water in bedding was the main factor to control the formation of interlayer karst reservoirs. In the karst process, faults controlled the groundwater runoff and drainage direction, i.e. determining the distribution of the karst fracture cave reservoirs. Based on the above results, a bedding karst model for the Xinken area was established to guide oil and gas exploration of the Ordovician system in this area.

     

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