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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2010  >  32(6): 547-552
Wang Furong, He Sheng, He Zhiliang, Zhang Fushun. THE RESERVOIR CHARACTERISTIC OF DEEPLY-BURIED SANDSTONE IN THE CENTER OF JUNGGAR BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(6): 547-552. doi: 10.11781/sysydz201006547
Citation: Wang Furong, He Sheng, He Zhiliang, Zhang Fushun. THE RESERVOIR CHARACTERISTIC OF DEEPLY-BURIED SANDSTONE IN THE CENTER OF JUNGGAR BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(6): 547-552. doi: 10.11781/sysydz201006547
shu

THE RESERVOIR CHARACTERISTIC OF DEEPLY-BURIED SANDSTONE IN THE CENTER OF JUNGGAR BASIN

doi: 10.11781/sysydz201006547
  • 1.

    Key Laboratory of Tectonics and Petroleum Resources (China University of Geosciences), Ministry of Education, Wuhan, Hubei 430074, China

  • 2. Faculty of Earth Resources, China University of Geosciences, Wuhan, Hubei 430074, China

  • 3. Exploration and Production Research Institute, SINOPEC, Beijing 100083, China

  • Received Date: 2010-03-12
  • Rev Recd Date: 2010-10-08
  • Publish Date: 2010-12-28
    Abstract
  • Many discovered petroleum mainly develop in the deeply-buried Jurassic and Cretaceous sandstone reservoirs in the center of Junggar Basin and intergranular secondary porosity develop at the depth of 3 500~6 200 m belong to a stage of late diagenesis. The porosity is about 4%~20% resulting from organic acid that generates from hydrocarbon maturation dissolving carbonate cements and silicate. According to the relationship among temperature, depth and Ro (vitrinite reflectance), there exists the other small scale secondary porosity band vertically resulting from organic acid dissolving ferro carbonate cements at the depth of 6 500 m.

     

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