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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2005-02
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Factors affecting reservoir properties of Upper Paleozoic in Ordos basin

ZHU Hong-quan~(1,2), XU Hong-jie~3(1.College of Energy Resources, Chengdu University of Technology, Chengdu 610059, China; 2.Institute of Oil and Gas Exploration and Development, Southwest Branch of SINOPEC, Chengdu 610081, China; 3.Northeast Project Managment Department of New Area Exploitation of SINOPEC, Beijing 100723, China)  
The Upper Paleozoic reservoirs in the north of Ordos basin are mainly composed of the sandstones of Shanxi and Xiashihezi Formations. Being densely compacted and of low permeability, they are generally considered low quality reservoirs. From south to north, the grain-size increases and the matrix content decreases while the sandstones get nearer to the source region. The reservoir properties improve gradually northward because of the weaker compaction and cementation. The reservoir properties display a trend of improvement upwards while the strata get newer and the sedimentary facies change from deltaic front to deltaic plain and to fluvial. So the characteristics that the property of the Upper Paleozoic reservoir in the north of Ordos basin degrades southward are mainly the result of the variation in the sedimentary facies and diagenesis.
【CateGory Index】: TE122.23
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