鄂尔多斯盆地西缘中南段构造特征与演化
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摘要
利用平衡地质剖面技术和2D Move软件对鄂尔多斯盆地西缘中南段骨架地震剖面进行了精细解释。重新厘定9条一级断裂,确定4个一级构造单元,依据地质结构与构造样式的不同,将西缘中南段划分为5个段。构造变形自西向东依次减弱,南北向中部马家滩段以薄皮构造为主,其余段以厚皮构造为主;西缘中南段不同地区最短收缩量不同,甜水堡段最短收缩量达50.62%,其构造变形主要发生于侏罗纪末期,最终定型于新生代。可见,西缘中南段具有"东西分带、南北分段"的典型特点,构造圈闭与油气聚集关系密切。
Main seismic sections in the west margin of the Ordos Basin are explained,depend on balanced section technology and 2D Move software.Nine first-level faults and four first-level structure units are confirmed,and the west margin of the Ordos Basin is divided into five sections.The structure distortion is stronger in the east than in the west.Majiatan section is thin-skinned structure,but the others are thick-skinned tectonics.The shortest compressed measure is different in different areas.Tianshuibu section's shortest compressed measure is up to 50.62%.Structure distortion came into being in Late Jurassic(146-135 Ma) mostly,ended in Cenozoic.Structure trap types are multiplex,which can supply a certain amount of space for the accumulation of oil and gas.Their forming matches with the period of accumulation of oil and gas.The structure character of the west margin of the Ordos Basin is different from east to west or from north to south.The relationship between the structure trap and accumulation of oil and gas is close.
引文
[1]丁超,陈刚,李振华,等.鄂尔多斯盆地东北部构造热演化史的磷灰石裂变径迹分析[J].现代地质,2011,25(3):581-589.
    [2]邓军,王庆飞,高帮飞,等.鄂尔多斯盆地演化与多种能源矿产分布[J].现代地质,2005,19(4):538-545.
    [3]刘和甫,李小军,刘立群.地球动力学与盆地层序及油气系统分析[J].现代地质,2003,17(1):80-86.
    [4]赵忠英,柳广弟,孙明亮,等.鄂尔多斯盆地上古生界天然气藏类型辨析[J].现代地质,2010,24(4):703-708.
    [5]郭振华,陈红汉,赵彦超,等.利用储层流体包裹体确定鄂尔多斯盆地塔巴庙区块上古生界油气充注期次和时期[J].现代地质,2007,21(4):712-719.
    [6]Suppe J.Geometry and kinematics of fault-bend folding[J].American Journal of Science,1983,283:684-721.
    [7]Suppe J,Medwedeff D A.Geometry and kinematics of fault-propagation folding[J].Eclogae Geologicae Helvetiae,1990,83(3):409-454.
    [8]Chapman T,Willlams G.Strains developed in the hanging wallsof thrusts due to their slip/propagation rate,a dislocation model[J].Journal of Structural Geology,1985,7(6):759-762.
    [9]Willlams R Jamison.Geometry analysis of fold development inoverthrust terranes[J].Journal of Structural Geology,1987,9(2):207-219.
    [10]陈剑,卢华复,王胜利.库车断层相关褶皱的切角检验[J].地质论评,2002,48(1):74-79.
    [11]何登发,John Suppe,贾承造.断层相关褶皱理论与应用研究新进展[J].地学前缘,2005,12(4):353-364.
    [12]Shaw J H,Connors C,Suppe J.Seismic Interpretation of Con-tractional Fault-Related Folds:An AAPG Seismic Atlas[M].Tulsa:American Association of Petroleum Geologists,2004:1-270.
    [13]何登发,周路,雷振宇,等.断层相关褶皱原理在前陆冲断带构造建模中的应用[M]//中国石油勘探与生产分公司.中国中西部前陆盆地冲断带油气勘探文集.北京:石油工业出版社,2002:210-228.

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