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Micro-anisotropic Experimental Analysis on Chang-8 Sandstone in Xifeng Area of Ordos Basin[J]. Rock and Mineral Analysis, 2008, 27(1): 29-32.
Citation: Micro-anisotropic Experimental Analysis on Chang-8 Sandstone in Xifeng Area of Ordos Basin[J]. Rock and Mineral Analysis, 2008, 27(1): 29-32.
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Micro-anisotropic Experimental Analysis on Chang-8 Sandstone in Xifeng Area of Ordos Basin

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  • Received Date: June 28, 2007
  • Revised Date: September 02, 2007
    Abstract
  • Based on the micro-model experiments for authentic sandstone samples, the micro-anisotropic characteristics of Chang-8 sandstones from the reservoirs in Xifeng area of Ordos Basin was analyzed. The results show that Chang-8 reservoirs behmg to compact-type sandstone with intense miero-anisotropy. And the diagenesis and porous structure of the sandstones are the main factors leading to the mieroanisotropy of Chang-8 reservoirs. The low permeable sandstones result in the intense mieroanisotropy of Chang-8 sandstone and form the high permeable zone of Chang-8 reservoirs.
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