摘要
Sedimentary process,X-rays fluorescence analysis of sandstone and mudstone,and reservoir characteristics analyzing were used in measuring the strata of Kapushaliang outcrop in Kuqa foreland basin. There are some solution opening in sandstones of tuibidite fan channel and lacustrine bar,but the solution value of lacustrine bar is higher than turbidite fan channel.The discovery of turbidite fan in Kapushaliang outcrop of Yageliemu Formation is important for foreland basin research in Kuqa,and instructs lacustrine deep water region development in the western Kuqa depression.