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塔里木盆地西南坳陷周缘的滑脱构造
引用本文:王步清,谢会文,陈汉林,王清华,杨宝俊.塔里木盆地西南坳陷周缘的滑脱构造[J].地质科学,2011,0(3):733-742.
作者姓名:王步清  谢会文  陈汉林  王清华  杨宝俊
作者单位:1.中国石油塔里木油田分公司 新疆库尔勒 841000;2.湘江大学地球科学系 杭州 310027;3.吉林大学地球探测科学与技术学院 长春 130026
基金项目:国家重点基础研究计划项目
摘    要:西南坳陷主要发育两套滑脱层序,一套是中寒武统和田河组膏盐岩,另一套是古近系底部阿尔塔什组和齐姆根组的夹灰岩、白云岩的膏泥岩;前者厚度500 m左右,后者厚度在100 ~700 m左右.和田河组膏盐岩主要影响中生代及中新世末的构造变形,古近系底部的膏泥岩主要影响上新世末及第四纪的构造变形,构造变形样式均以顺层滑脱构造为主...

关 键 词:塔里木盆地  西南坳陷  膏泥岩  滑脱构造  断层相关褶皱
收稿时间:2011-03-10

Decollement structure of southwest Tarim depression and its periphery
Wang Buqing,Xie Huiwen,Chen Hanlin,Wang Qinghua,Yang Baojun.Decollement structure of southwest Tarim depression and its periphery[J].Chinese Journal of Geology,2011,0(3):733-742.
Authors:Wang Buqing  Xie Huiwen  Chen Hanlin  Wang Qinghua  Yang Baojun
Institution:1.Tarim Oilfield Company, PetroChina, Korla, Xinjiang 841000;2.Department of Earth Sciences, Zhejiang University, Hangzhou 310027;3.College of Geoexploration Science and Technology, Jilin University, Changchun 130026
Abstract:There are two decollement strata in southwestern depression of Tarim Basin:one is 500 m Middle Cambrian salt gypsum layer,and another is 100~700 m Lower Paleogene gypsum mudstone with limestone and dolostone.The Middle Cambrian salt gypsum layer is mainly related with Mesozoic and Late Miocene structural deformation,however,the Lower Paleogene gypsum mudstone is mainly involved in Late Pliocne and Quaternary structural deformation.The decollement structure is the most important structural style.The decollement structure and other structural styles consist of four kinds of structural assemblages in section: 1)decollement fault related fold; 2)imbricated decollement structure; 3)wedging structure+reconstructed fault related fold; 4)detachment fault+fault related fold.The former two structural assemblages mainly distribute in Maigaiti slope and its periphery,and the latter two structural combinations mainly distribute in fold and thrust belt of western Kunlun Mountain.The structural modes of these structural styles are set up,which are significant to structural interpretation and identification of traps of complicated areas in southwest Tarim Basin.
Keywords:Tarim Basin  Southwest depression  Gypsum mudstone  Decollement structure  Fault-related fold
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