LITHOLOGIC RESERVOIRS ›› 2015, Vol. 27 ›› Issue (5): 196-203.doi: 10.3969/j.issn.1673-8926.2015.05.032

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Formation mechanism of sand bodies of the eighth member of Shihezi Formation in northern Ordos Basin

Liu Xiaopeng12, Zhao Xiaohui12, Kang Rui12, Qi Yaling12   

  1.  1. Research Institute of Exploration and Development , Petrochina Changqing Oilfield Company , Xi ’ an 710018 , China ; 2. National Engineering Laboratory for Low Permeability Oil and Gas Fields Exploration and Development , Xi ’ an 710018 , China
  • Online:2015-09-26 Published:2015-09-26

Abstract:

In order to clarify the formation mechanism of sand bodies in the eighth member of Permian Shihezi Formation in the northern Ordos Basin, the sedimentary palaeoenvironments including basin character, the connectivity of lake and the outside world, provenance supply and hydrodynamic force conditions were recovered on the base of the characteristics of sand body distribution. Combined with the sedimentary simulation, the sedimentary model of the eighth member of Shihezi Formation was established. The result shows that sufficient sediment supply, strong hydrodynamic force, abundant clastic supplying by several rivers, broad flat topography, stable and rapid basin subsidence and lake level fluctuate with large range are the main factors responsible for the large-area sand bodies of the eighth member of Shihezi Formation. The area from the north of L63 well, S318 well, Y101 well and Y112 well to south of Etuokeqianqi-Yulin area in Ordos Basin is the favorable target for exploration in the future.

Key words: seismic sedimentology , thin sand body , spectrum decomposition, phase transform , strata slice, seismic attributes

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