塔里木盆地北部跃南断裂带的形成演化

周慧, 黄理力, 龚洪林, 刘亚雷, 文磊, 李曰俊. 2021. 塔里木盆地北部跃南断裂带的形成演化. 地质科学, 56(3): 730-739. doi: 10.12017/dzkx.2021.036
引用本文: 周慧, 黄理力, 龚洪林, 刘亚雷, 文磊, 李曰俊. 2021. 塔里木盆地北部跃南断裂带的形成演化. 地质科学, 56(3): 730-739. doi: 10.12017/dzkx.2021.036
Zhou Hui, Huang Lili, Gong Honglin, Liu Yalei, Wen Lei, Li Yuejun. 2021. The formation and evolution of the Yuenan fault belt in the northern Tarim Basin. Chinese Journal of Geology, 56(3): 730-739. doi: 10.12017/dzkx.2021.036
Citation: Zhou Hui, Huang Lili, Gong Honglin, Liu Yalei, Wen Lei, Li Yuejun. 2021. The formation and evolution of the Yuenan fault belt in the northern Tarim Basin. Chinese Journal of Geology, 56(3): 730-739. doi: 10.12017/dzkx.2021.036

塔里木盆地北部跃南断裂带的形成演化

  • 基金项目:

    中国石油天然气股份有限公司十三五专项“古老碳酸盐岩的油气成藏分布规律与关键技术”(编号:2019B-04)资助。

详细信息
    作者简介:

    周慧,男,1983年生,博士,高级工程师,石油地质学专业。E-mail:zhouhui03@petrochina.com.cn

  • 中图分类号: P541;P542

The formation and evolution of the Yuenan fault belt in the northern Tarim Basin

  • 跃南断裂带是塔里木盆地北部的一条形状奇特的断裂带,平面展布呈口袋状。在系统的地震资料解释的基础上,通过认真的断裂构造分析,认为跃南断裂带经历了二叠纪、二叠纪末—三叠纪和侏罗—白垩纪3期断裂作用的叠加。二叠纪大陆裂谷作用形成的一系列NE-SW和NW-SE走向的陡倾的正断层,组成一个共轭断裂系统。沿跃南断裂带的两组不同方向的正断层活动加强,并最终追踪、贯通,形成了口袋状的跃南断裂带。也就是说,跃南断裂带实际上是由NE-SW和NW-SE走向两组断层组合而成的。断裂带围限的地块相对抬升,形成一个大型的垒块。二叠纪末—三叠纪南天山碰撞造山作用引起的逆冲断层,叠加在二叠纪正断层之上,进一步强化了跃南断裂带,使之断距加大,围限的垒块进一步抬升。侏罗—白垩纪的正断层属于南天山造山后的伸展构造,见于跃南断裂带上方,规模不大,数量不多,对断裂带有一定的调整作用。
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收稿日期:  2020-10-15
修回日期:  2021-01-25
刊出日期:  2021-09-01

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