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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2014  >  36(4): 416-421
Qiao Guilin, Qian Yixiong, Cao Zicheng, Yue Yong, Zhang Yongdong, Yang Zhongliang. Reservoir characteristics and karst model of Ordovician Yingshan Formation in Yubei area, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(4): 416-421. doi: 10.11781/sysydz201404416
Citation: Qiao Guilin, Qian Yixiong, Cao Zicheng, Yue Yong, Zhang Yongdong, Yang Zhongliang. Reservoir characteristics and karst model of Ordovician Yingshan Formation in Yubei area, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(4): 416-421. doi: 10.11781/sysydz201404416
shu

Reservoir characteristics and karst model of Ordovician Yingshan Formation in Yubei area, Tarim Basin

doi: 10.11781/sysydz201404416
  • 1.

    Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • 2. Research Institute of Petroleum Exploration and Development, SINOPEC Northwest Oilfield Company, Urumqi, Xinjiang 830011, China

  • 3. Prospecting Institute, Guangdong Bureau of Coal Geology, Guangzhou, Guangdong 510440, China

  • Received Date: 2013-03-13
  • Rev Recd Date: 2014-06-07
  • Publish Date: 2014-07-28
    Abstract
  • By means of core observation, statistics of pore, hole and fraction, logging, and diagenesis, researches are carried out, indicating that the reservoir space types and property of the weathering crust of the Ying-shan Formation are different among different structures in the Yubei area. The superposition of multi-period karst took place in the weathering crust of the north-east trending structure in the Yubei area, and the reservoir spaces such as cave, hole and fracture developed, showing good reservoir property. In the Pingtai area and the Yudong fault depression, only the middle Caledonian stage Ⅰ karsts generated with poorer reservoir property, mainly of fractures and weak solution pores. Because of dolomitization, bedding solution pore and fracture reservoirs deve-loped in karst insider of the lower member of the Yingshan Formation, and pores and holes occurred alone, showing poor connectivity and no/half filling (oil or calcite). The evolution models of the Yingshan Formation karst reservoirs were established. And the tectonic movement of the middle-late Caledonian and early Hercynian controlled ancient landform and influenced the karst reservoir development in the Yabei area.

     

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