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《Progress in Geophysics》 2011-01
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High-frequency carbonate depositional cycles and its response to the gamma ray well logging data and sea-level change in Permian Nanpanjiang Basin

GONG Da-xing~1,YI Hai-sheng~(1,2),WU Chi-hua~1,TANG Yun-feng~1(1.Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,China;2.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu 610059,China)  
The method of Fischer plots,which is used to identify the carbonate sedimentary sequence,define longperiod sea-level change,is just used in the fields of outcrop or drill core.Similarly,the way to recognize highfrequency depositional cycles still relys on manpower.Now,by virtue of gamma ray well logging data,using the first difference method and Fischer plots,431 high-frequency depositional cycles can be identified from the isolated carbonate platform in the area of Yang 1 well,in Permian Nanpanjiang basin.The thickness of these cycles change form 0.25 m to 4.25 m,the average value is 1.5m.And 6 times third-order sea-level fluctuations could be defined in the time of lower Premian in this area,the early of Maokou has been confirmed as the period of maximum flooding surface.
【Fund】: “十一五”国家科技支撑计划项目(2006BAB01A12-5)资助
【CateGory Index】: P631.81;P731.23
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