J4 ›› 2009, Vol. 39 ›› Issue (5): 781-788.

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Relationship of Sandstone Diagenesis and Relatively High Porosity Areas in Nantun and Tongbomiao Formation: A Case from the Southern of Wuerxun Depression in Hailaer Basin

YOU Li1|LI Chun-bai2|LIU Li3|LI Cai1,WANG Hai-yan4   

  1. 1.Zhanjiang Branch,China National Offshore Oil Limited Corporation-Zhanjiang, Zhanjiang,Guangdong 524057, China;2.Exploration and Development Research Institute, Daqing Oil Field Ltd. Co., Daqing, Heilongjiang 163712, China;3.College of Earth Sciences, Jilin University,Changchun 130061, China;4.Zhanjiang Nanhai-West Research Institute,China National Offshore Oil Corporation Energy Technology &|Services,Zhanjiang,Guangdong 524057,China
  • Received:2008-12-16 Online:2009-09-26 Published:2009-09-26

Abstract:

The types of sandstone from Nantun and Tongbomiao Formation of Wuerxun depression in Hailaer basin are mainly debris-feldspar sandstone, sightly feldspar sandstone and feldspar-debris sandstone. The diageneses include compaction, cementation, metasomatism and dissolution, etc. With depth increasing, the porosity and permeability decrease. There are four relatively high porosity arears in about 1 500 m,1 850-2 050 m,2 300 m and 2 600-2 800 m. The reasons of relatively high porosity areas appearance are the preservation of primary porosity and the development of secondary porosity.The weakness of compaction and cementation, existence of clay coating and microcrystalline quartz are favor to the preservation of primary porosity；in the processing of thermal evolution of organic content and the conversion of clays, secondary porosity forming occurs.

Key words: Hailaer basin, sandstone, relatively high porosity areas, preservation of primary porosity, secondary porosity forming

CLC Number: 

  • P618.13
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