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Zhang Boquan;Guan Zhenliang;Pan Lin(Department of Petroleum Geology,China University of Geosciences,Wuhan 430074)  
The results obtained from the compactional studies by means of the microscope observation of sections,a compaction curve of porosity vs depth and the simulating experiments of carbonate rocks in Ordos basin at high-temperature and-pressure suggest the compaction,especially mechanical compaction exists in the carbonate rocks.Three compactional stages can be distinguished in this area.
【Fund】: “八五”国家重大科技攻关项目
【CateGory Index】: P54
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