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《Progress in Geophysics》 2007-02
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Physical model and seismic recognition of concealed volcanic edifices of Yingcheng Formation in Songliao Basin,Cretaceous,NE China

TANG Hua-feng1,WANG Pu-jun1,JIANG Chuan-jin2,BIAN Wei-hua1,HUANG Yu-long1(1.College of Earth Sciences,Jilin University,Changchun 130061,China;2.Daqing Exploration &Development Institute,Daqing 163712,China)  
Volcanic edifice is divided into three facies belts which are crater-near crater facies(CNCF),proximal facies(PF) and distal facies(DF).The dip ranges of the three facies belts in outcrops are listed: CNCF-40~70°,PF-25~45°,DF-20~35°.The liner density of fracture of the three facies belts are listed: CNCF-10~30 fractures per meter,PF-3~25 fractures per meter,DF-2~11 fractures per meter.The coherent value relation of the three facies belts is CNCFPFDF.Both dip angle and coherence cube methods are selected to recognize the buried volcanic edifices in Songliao Basin.Fourteen volcanic edifices are recognized in both two methods in the first volcanic cycle of Yingcheng Formation and the prediction perfectly corresponds to the drilling results in well XS8-well XS4 area.Successful ratio of wells attains 90% when the prediction results are employed in the exploration of Qingshen gas field.
【Fund】: 国家重点基础研究发展计划(973计划)项目(2006CB701403);; 国家自然科学基金面上项目(40372066号)联合资助
【CateGory Index】: P631
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