Lithologic Reservoirs ›› 2014, Vol. 26 ›› Issue (6): 69-74.doi: 10.3969/j.issn.1673-8926.2014.06.012

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Quantification of late Paleogene uplift in Nanyang Sag using acoustic velocity

WANG Zhongnan1, LIU Guangdi1, CHEN Wan2, YANG Yuran3, GUO Feifei4, TANG Hui5
  

  1.  1. College of Geosciences , China University of Petroleum , Beijing 102249 , China ; 2. No. 3 Oil Production Plant , PetroChina Daqing Oilfield Company , Daqing 163458 , Heilongjiang , China ; 3. Research Institute of Exploration and Development , PetroChina Southwest Oil and Gas Field Company , Chengdu 629000 , China ; 4. Postdoctoral Research Institute , Henan Oilfield Company , Sinopec , Nanyang 473132 , Henan , China ; 5. PetroChina Research Institute of Petroleum Exploration and Development , Beijing 100083 , China
  • Online:2014-11-20 Published:2014-11-20

Abstract:

The abnormal pressure is not common in Liaozhuang Formation and the first member of Hetaoyuan Formation in Nanyang Sag, and acoustic velocity is mainly controlled by maximal historical burial depth. Typical wells that located in the center and the margin of the sag were selected to investigate the relationship between acoustic velocity and depth of mudstone of Liaozhuang Formation and the first member of Hetaoyuan Formation, and then the uplift of the late Paleogene was qualified based on velocity-depth trend and velocity data. The result shows that the uplift ranges from 400 m to 1 000 m, the uplift in the western and southern part is relatively low and it increased gradually toward the northeast to about 1 000 m. Based on the analysis of horizontal distribution of uplift, it is considered that the large scale uplift near Weigang-Beimazhuang structural belt caused the occurrence of subnormal pressure. Decompression, increasing in volume and petroleum pumping function during uplift increase reservoirs space, forming lower potential area, thus contributes to oil and gas accumulation.

Key words:  tight sandstone , reservoir characteristics , sedimentation, He-1 member, Dingbei area

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