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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2018  >  40(2): 260-267
ZHAO Jun, CAO Qiang, FU Xiandi, ZHANG Feifei, ZHANG Feifei, QIN Guoying. Recovery of denuded strata thickness based on Milankovitch Astronomical Cycles: A case study of Qingshankou Formation in X Oilfield, Songliao Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(2): 260-267. doi: 10.11781/sysydz201802260
Citation: ZHAO Jun, CAO Qiang, FU Xiandi, ZHANG Feifei, ZHANG Feifei, QIN Guoying. Recovery of denuded strata thickness based on Milankovitch Astronomical Cycles: A case study of Qingshankou Formation in X Oilfield, Songliao Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(2): 260-267. doi: 10.11781/sysydz201802260
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Recovery of denuded strata thickness based on Milankovitch Astronomical Cycles: A case study of Qingshankou Formation in X Oilfield, Songliao Basin

doi: 10.11781/sysydz201802260
  • 1.

    No. 10 Oil Production Plant, PetroChina Daqing Oilfield, Daqing, Heilongjiang 166405, China

  • 2. Exploration and Development Research Institute, PetroChina Daqing Oilfield, Daqing, Heilongjiang 163618, China

  • 3. Faculty of Earth Resources, China University of Geosciences(Wuhan), Wuhan, Hubei 430074, China

  • Received Date: 2017-08-14
  • Rev Recd Date: 2018-01-29
  • Publish Date: 2018-03-28
    Abstract
  • The Milankovitch Astronomical Cycles were applied to study the erosion thickness of Qingshankou Formation (K2qn) in the X Oilfield, Songliao Basin. Spectral analysis and wavelet transform revealed that the Milankovitch Cycles occurred in the K2qn. We detected the eccentricity period of 100 ka, obliquity period of 40 ka and precession period of 20 ka in the K2qn. The bandpass filtering of 42 exploratory wells in the X Oilfield showed that, the K2qn has 35 to 43 eccentricity periods of 100 ka, which proved erosion phenomenon. The erosion thickness of K2qn is 0-98 m, and gradually decreases from northeast to southwest, where non-denuded areas distribute widely. Tectonic uplift and erosion took place regionally in the X Oilfield during or at the end of the sedimentation of K2qn.

     

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