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《Journal of Changchun University of Science and Technology》 2003-03
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DIFFERENTIATION OF FLUVIAL SEDIMENT SYSTEM OF THE QUANTOU FORMATION AND ITS DEPOSITIONAL CONDITION IN THE HELONG AREA OF SONGLIAO BASIN

FANG Shi1,LIU Zhaojun1,WANG Shaoshuang2,HUANG Xiangtong1(1.College of Earth Sciences,Jilin University, Changchun130061,China;2.Jilin Star Liquid Carbon Co. LTD, Chanchun130062,China)  
Based on timefrequency analysis, the well log was analysed depositionally in order to rationaly distinguish objects at the Qclustering analysis.Using timefrequency analysisCustering analysis, the sedimentary facies types of the upper part of the Quantou Formation in the Helong area of Songliao Basin were disfinguished.The result shows that member 3 Rbottom of Member 4 of the Quantou Formation is braided river depositional system and Member 4 of the Quantou Formation(besides its bottom) is meandering river deposition system,and that tectonic subsidence,rainfall,sloping,palaeovegetation and calcify beds are important factors to contral the existence and evolution of braided or meandering river.
【Fund】: 中国石油天然气总公司"九五"重点攻关项目资助(981707038)
【CateGory Index】: P343.1
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