塔里木盆地晚志留世—石炭纪伸展构造的发现及其地质意义

李曰俊, 孙龙德, 杨海军, 张光亚, 曾昌民, 冯晓军, 文磊, 张强, 贾铁干. 塔里木盆地晚志留世—石炭纪伸展构造的发现及其地质意义[J]. 地质科学, 2014, 49(1): 30-48. doi: 10.3969/j.issn.0563-5020.2014.01.003
引用本文: 李曰俊, 孙龙德, 杨海军, 张光亚, 曾昌民, 冯晓军, 文磊, 张强, 贾铁干. 塔里木盆地晚志留世—石炭纪伸展构造的发现及其地质意义[J]. 地质科学, 2014, 49(1): 30-48. doi: 10.3969/j.issn.0563-5020.2014.01.003
Li Yuejun, Sun Longde, Yang Haijun, Zhang Guangya, Zeng Changmin, Feng Xiaojun, Wen Lei, Zhang Qiang, Jia Tiegan. New discovery of Late Silurian-Carboniferous extensional structure in Tarim Basin and its geological significance[J]. Chinese Journal of Geology, 2014, 49(1): 30-48. doi: 10.3969/j.issn.0563-5020.2014.01.003
Citation: Li Yuejun, Sun Longde, Yang Haijun, Zhang Guangya, Zeng Changmin, Feng Xiaojun, Wen Lei, Zhang Qiang, Jia Tiegan. New discovery of Late Silurian-Carboniferous extensional structure in Tarim Basin and its geological significance[J]. Chinese Journal of Geology, 2014, 49(1): 30-48. doi: 10.3969/j.issn.0563-5020.2014.01.003

塔里木盆地晚志留世—石炭纪伸展构造的发现及其地质意义

详细信息
    作者简介:

    李曰俊,男,1962年7月生,博士,构造地质学和地层学专业。E-mail:yuejunleecheng@sina.com

  • 中图分类号: P542

New discovery of Late Silurian-Carboniferous extensional structure in Tarim Basin and its geological significance

  • 通过精细的地震资料解释,在塔里木盆地中部的满西地区发现晚志留世—石炭纪伸展构造。伸展构造由一系列规模不大的正断层组成,平面上组成两条北东—南西向的左行雁列状正断层带,剖面上构成负花状构造和堑垒构造。根据生长系数计算结果,正断层形成于晚志留世,在泥盆纪和石炭纪持续活动,于石炭纪末停止活动。正断层活动的高峰期为晚志留世。该期伸展构造在塔中和塔北地区也有发育,反映当时塔里木盆地处于区域性伸展构造背景。塔里木盆地晚志留世—石炭纪的伸展构造,是昆仑早古生代晚期(晚奥陶世—中志留世)碰撞造山后构造应力松弛作用的产物。
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收稿日期:  2013-05-06
修回日期:  2013-10-05
刊出日期:  2014-01-25

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