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歧口凹陷滩海区下第三系层序地层分析及沉积体系研究
引用本文:许淑梅,翟世奎,李三忠,周立宏.歧口凹陷滩海区下第三系层序地层分析及沉积体系研究[J].沉积学报,2001,19(3):363-367.
作者姓名:许淑梅  翟世奎  李三忠  周立宏
作者单位:1.青岛海洋大学 山东青岛 266003;
摘    要:利用地震、测井、岩心等资料,通过对该区进行层序地层学的分析和研究,把歧口凹陷滩海区下第三系划分出一个二级层序,六个三级层序,并对每个层序的主控成因进行了详细的研究,总结出构造层序和气候层序的不同特点。同时对每个层序内部的沉积特点和沉积体系进行了分析,指出了层序发育对岩石储集性的控制作用。研究过程中,还发现陆相盆地的单断特点控制了该区层序发育的总体特征;而断陷湖盆内部三级断层对层序内砂体的位置则有明显的控制作用。

关 键 词:歧口凹陷    断陷盆地    层序地层    沉积体系
文章编号:1000-0550(2001)03-0363-05
收稿时间:2000-06-17
修稿时间:2000年6月17日

An Analysis on Sequence Stratigraphy and Sedimentary System of Early Neocene in Qikou Sag
XU Shu mei,ZHAI Shi kui,LI San zhong,ZHOU Li hong.An Analysis on Sequence Stratigraphy and Sedimentary System of Early Neocene in Qikou Sag[J].Acta Sedimentologica Sinica,2001,19(3):363-367.
Authors:XU Shu mei  ZHAI Shi kui  LI San zhong  ZHOU Li hong
Institution:1.Department of Marine Geology, Ocean University of Qingdao,Qingdao Shandong 266003;2.Dagang Oilfield Group Ltd Company,Dagang Tianjin 300280
Abstract:The paper discusses the features of Early Neocene's sequence stratigraphy and sedimentary system of Qikou sag by employing large mount of materials such as seismic data, logging data, observation results of rock cores and new rule. There are one secondary sequence and six third level sequences of Early Neocene in Qikou sag. Based on studies of controlling factors of sequence development, we conclude that there are two kinds of sequence developed in Qikou sag, which are tectonic sequence and climate sequence. Sequence 1, sequence 3,sequence 4, sequence 5 and sequence 6 are tectonic sequence because the action of the boundary faults controls the space of sedimentation. Sequence 2 is the climate sequence. During the sedimentation of sequence 2, the primary controlling factor on the sequence model is climate and the changes of lake level are not influenced by the uplift of basement rock and the action of boundary faults. During progression period, fan head, mid fan and far end of alluvial fan or fan delta developed on different fault terraces, turbidity fan and gravity flow deposits developed in deeply depressed position. During high stand, wedge and lenses shaped deposits of delta occured on the whole basin. The development of sequence controls the rock's reservoir proporty. The sag's tectonic feature influences the distribution of the sequence and the third level fault has eminent influence on sand bodies. For example, fan head, mid fan and far end of alluvial fan or fan delta developed near the lower part of the faults. These findings could be used to predict the location of sand bodies and have great significances in directing the petroleum exploration.
Keywords:Qikou sag  faulted depression  sequence stratigraphy  sedimentary system
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