塔里木盆地西北缘沙井子构造带断裂构造分析

齐英敏, 李曰俊, 王月然, 刘亚雷, 朱海燕, 刘立炜, 莫涛, 陈延贵. 塔里木盆地西北缘沙井子构造带断裂构造分析[J]. 地质科学, 2012, 47(2): 265-277.
引用本文: 齐英敏, 李曰俊, 王月然, 刘亚雷, 朱海燕, 刘立炜, 莫涛, 陈延贵. 塔里木盆地西北缘沙井子构造带断裂构造分析[J]. 地质科学, 2012, 47(2): 265-277.
Qi Yingmin, Li Yuejun, Wang Yueran, Liu Yalei, Zhu HaiyanLiu, Liu Liwei, Mo Tao, Chen Yangui. Fault analysis on Shajingzi structural belt, NW margin of Tarim Basin, NW China[J]. Chinese Journal of Geology, 2012, 47(2): 265-277.
Citation: Qi Yingmin, Li Yuejun, Wang Yueran, Liu Yalei, Zhu HaiyanLiu, Liu Liwei, Mo Tao, Chen Yangui. Fault analysis on Shajingzi structural belt, NW margin of Tarim Basin, NW China[J]. Chinese Journal of Geology, 2012, 47(2): 265-277.

塔里木盆地西北缘沙井子构造带断裂构造分析

详细信息
  • 中图分类号: P542

Fault analysis on Shajingzi structural belt, NW margin of Tarim Basin, NW China

  • 沙井子构造带位于塔里木盆地西北缘,是分隔阿瓦提凹陷和温宿凸起的边界断裂。它是塔里木盆地研究最薄弱的大型断裂构造带之一。根据系统、精细的地震资料解释,沙井子构造带存在3套断裂体系:深部楔状冲断构造、狭义沙井子断裂和浅部的伸张构造。深部楔状冲断构造形成于志留纪—泥盆纪,由北西倾向的主冲断层和南东倾向的反冲断层形成构造楔; 构造楔主要由前寒武纪变质岩组成,冲断前锋楔入于寒武系中部,造成上覆地层向温宿凸起方向的急剧抬升。狭义的沙井子断裂,即通常所说的沙井子断裂,为一条高角度基底卷入型挤压走滑断裂,形成于二叠纪末—三叠纪初,错断了早期的深部冲断楔。浅部的伸展构造形成于第四纪早-中期,为一系列较小规模的正断层,沿狭义沙井子断裂呈右步雁列状排列,构成左行剪切张扭性断裂带。深部的楔状冲断构造和浅部的伸展构造是本次研究的新发现。
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出版历程
收稿日期:  2011-10-15
修回日期:  2011-12-15
刊出日期:  2012-04-25

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