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The Diagenesis of Chang-8 Reservoir Sandstone and Its Effect on Porosity in Xifeng Oilfield

YU Bo1,CUI Zhi-lin1,LIU Xue-gang2,QIAN Li-dan3,BAI Chang-e2,ZHU Tao1   

  1. 1.Department of Geology/State Key Laboratory of Continental Dynamic, Northwest University, Xi’an 710069,China;2.Research Institute of Exploration and Development, Changqing Oil Field,Xi’an 710021,China;3.Research Institute of Exploration and Production,Xinjiang Oilfield Company,Kelamayi,Xinjiang 834011,China
  • Received:2007-10-12 Revised:1900-01-01 Online:2008-05-26 Published:2008-05-26
  • Contact: YU Bo

Abstract: Based on the analysis of thin-section, casting lamella, scanning electron microscope,X-ray diffractions and so on,the characteristic of petrology and the diagenesis of Chang-8 reservoir in Xifeng oilfield in the Ordos Basin was summarized. The result shows that both feldspathic litharenite and lithic arkose are the essential components of Chang-8 sandstone. The diagenesis is in the early A period of the late diagenesis stage. The compaction in the early stage and a number of minerals’ cementation lead the loss of primary porosity, the dissolution is the main diagenesis to form second porosity.

Key words: Xifeng oilfield, diagenesis, porosity

CLC Number: 

  • P618.13
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