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Geoscience ›› 2014, Vol. 28 ›› Issue (5): 1017-1022.

• Energy Geology • Previous Articles     Next Articles

Study on the Influence of Strike-slip Fault Displacement on Reservoir in Northern Slope, Tazhong Area

ZHANG Xin-chao1,2, SUN Zan-dong2, ZHAO Jun-sheng2, PAN Yang-yong3, WU Mei-zhen3   

  1. (1.Postdoctoral Research Institute of Henan Oilfield Company,SINOPEC, Nanyang,Henan473132,China; 2.Lab for Integration of Geology and Geophysics (LIGG), China University of Petroleum, Beijing102249,China; 3.Petroleum Exploration and Development Research Institute of Tarim Oilfield Company, PetroChina, Korla, Xinjiang841000,China)
  • Online:2014-10-25 Published:2014-12-29

Abstract:

Reservoir reformation and petroleum distributions in Ordovician carbonate reservoirs are affected by strike-slip faults with northeast direction in the Northern Slope of Tazhong area. Large scale strike-slip faults always show north-east strike direction. Unfortunately, the horizontal displacement is too shorter to be identified by using poor quality and low resolution seismic data. Strike-slip faults show ubiquitous pullapart areas along the strike direction, because they have been affected by the tensional stress with northwest direction. And pull-apart areas are developed along the direction of strike-slip faults mainly affected by the formation of local stresses. The width and height of these areas are easy to be identified in 3D seismic data. A method is then proposed for displacement calculation by using the width and height of the pull-apart area to replace the horizontal displacement and vertical displacement of fault. Displacement calculation results by this method show a high agreement to geology regularity of strike-slip faults development. Large displacement in strike-slip faults always means a high activity regional area, and also shows a profitability area for reservoir reformation or petroleum accumulation.

Key words: the Northern Slope of Tazhong area, strike-slip fault, displacement, pull-apart area, petroleumdistribution

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