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    冀冬生, 甘仁忠, 庞志超, 李静, 王心强, 李全皓, 2025. 天山北麓中生代构造特征及其对新生代变形的意义. 地球科学. doi: 10.3799/dqkx.2025.168
    引用本文: 冀冬生, 甘仁忠, 庞志超, 李静, 王心强, 李全皓, 2025. 天山北麓中生代构造特征及其对新生代变形的意义. 地球科学. doi: 10.3799/dqkx.2025.168
    Ji Dongsheng, Gan Renzhong, Pang Zhichao, Li Jing, Wang Xinqiang, Li Quanhao, 2025. Mesozoic structure and its impact on Cenozoic deformation in the Northern Piedmont of Tianshan Mountain. Earth Science. doi: 10.3799/dqkx.2025.168
    Citation: Ji Dongsheng, Gan Renzhong, Pang Zhichao, Li Jing, Wang Xinqiang, Li Quanhao, 2025. Mesozoic structure and its impact on Cenozoic deformation in the Northern Piedmont of Tianshan Mountain. Earth Science. doi: 10.3799/dqkx.2025.168

    天山北麓中生代构造特征及其对新生代变形的意义

    doi: 10.3799/dqkx.2025.168
    基金项目: 

    中国石油天然气股份有限公司科技重大专项“超深层碎屑岩油气规模增储上产与勘探开发技术研究”(2023ZZ14)和“致密气新区新领域资源潜力与富集规律研究”(2021DJ2101)资助

    详细信息
      作者简介:

      冀冬生(1981—),男,2010年获长江大学硕士学位,现为中国石油新疆油田公司勘探开发研究院高级工程师,从事复杂构造油气勘探研究工作。Email:sxytjds@petrochina.com.cn。

      通讯作者:

      李全皓(1999—),男,硕士生,主要从事构造地质学工作。Email:2743946320@qq.com。

    • 中图分类号: TE132

    Mesozoic structure and its impact on Cenozoic deformation in the Northern Piedmont of Tianshan Mountain

    • 摘要: 天山北麓褶皱冲断带经历了多期构造运动,于晚新生代收缩作用下定型,多期叠合作用下,基底构造对后续挤压构造的影响并不明确。本文基于高精度三维地震和钻井资料,结合野外地质观测,研究天山北麓中生代构造特征和变形机理,以揭示中生代构造对新生代变形和油气运聚的影响和控制因素。研究认为天山北麓中生代发育走滑断层,被白垩系-新生界覆盖。中生代走滑断裂在晚新生代挤压环境下重新激活,其上覆叠加了新生代逆冲断裂和褶皱,中生代构造的重新激活对塑造天山及其天山北麓现今构造发挥了重要作用。依据构造变形期次,将准噶尔盆地南缘的沉积层划分为浅、中、深三个构造层,对应上、中、下三套油气成藏组合,其中,中、深构造层具有较大勘探潜力。本文揭示天山北麓深部断层与后期挤压构造的关系,明确多期构造叠合演化对油气勘探的影响,对中国西部盆地类似构造研究提供借鉴。

       

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    • 收稿日期:  2025-05-21
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