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《Journal of Oil and Gas Technology》 2009-03
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Sedimentary Characteristics and Mode of Shallow Delta in Large Scale Downwrap Lacustrine Basin——By Taking Quan-4 Formation in Maoxing and Aonan Region in Songliao Basin for Example

HU Ming-yi, MA Yan-rong, LIU Xian-qing, WANG Hui, WANG Yan-qi (College of Geosciences, Yangtze University, Jingzhou 434023,Hubei,China)  
Quan-4 member of Songliao Basin was mainly consisted of mudstone, silty mudstone and siltstone, which was included less fine sandstone sediments. By analyzing the characteristics of mudstone colors, fossils, granularity distribution and sedimentary structures, Quan-4 member in the studied area is confirmed as shallow delta depositional system.It develops delta plain and delta front subfacies, distributary channel and crevasse channel are the main characteristics, which reflects channel bifurcation and crevasse transformation. Based on this, The distribution maps of sedimentary microfacies of Maoxing and Aonan are drawn and the shallow delta depositional model of this region is established, it provides geologic foundation for farther exploration and development in Fuyu Reservoir.
【CateGory Index】: P618.13
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