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银川盆地东缘黄河断裂展布特征新认识

虎新军, 陈晓晶, 李宁生, 仵阳, 陈涛涛. 2021. 银川盆地东缘黄河断裂展布特征新认识. 物探与化探, 45(4): 913-922. doi: 10.11720/wtyht.2021.1445
引用本文: 虎新军, 陈晓晶, 李宁生, 仵阳, 陈涛涛. 2021. 银川盆地东缘黄河断裂展布特征新认识. 物探与化探, 45(4): 913-922. doi: 10.11720/wtyht.2021.1445
HU Xin-Jun, CHEN Xiao-Jing, LI Ning-Sheng, WU Yang, CHEN Tao-Tao. 2021. New understanding of the distribution characteristics of the Yellow River fault on the eastern margin of Yinchuan Basin. Geophysical and Geochemical Exploration, 45(4): 913-922. doi: 10.11720/wtyht.2021.1445
Citation: HU Xin-Jun, CHEN Xiao-Jing, LI Ning-Sheng, WU Yang, CHEN Tao-Tao. 2021. New understanding of the distribution characteristics of the Yellow River fault on the eastern margin of Yinchuan Basin. Geophysical and Geochemical Exploration, 45(4): 913-922. doi: 10.11720/wtyht.2021.1445

银川盆地东缘黄河断裂展布特征新认识

  • 基金项目:

    宁夏回族自治区重点研发计划重大(重点)项目(2018BFG02012)

    宁夏深部探测方法研究示范创新团队项目(KJT2019005)

    宁夏自然科学基金项目(2020AAC03449)

详细信息
    作者简介: 虎新军(1987-),男,宁夏银川市人,工程师,主要从事地球物理勘探研究工作。Email:junyan_home@126.com
  • 中图分类号: P631

New understanding of the distribution characteristics of the Yellow River fault on the eastern margin of Yinchuan Basin

  • 作为宁夏北部重要的区域性断裂之一,黄河断裂控制了银川新生代断陷盆地形成与演化,是研究银川平原地震活动及地热资源富集规律不可避免的关键点之一。目前,专项针对黄河断裂的研究较少,以地表调查为主,局部地区开展了浅层地球物理勘探。本文以地质露头资料为线索,基于区域1:20万重力资料,利用小波分界、斜导数等地球物理数据处理技术,清晰刻画出黄河断裂具有“雁行式平面展布特征,据此将断裂划分为灵武段、临河段、月牙湖段与礼和段4个亚段;临河段与灵武段的CSAMT资料揭示黄河主断裂及其次级断裂由东向西呈逐级下掉的“阶梯状,具有明显的“分级特征。黄河主断裂下切深度直抵上地壳,剖面上与次级规模断裂组合形态呈现典型的“扫帚状,各条断裂“上陡、中缓、下陡的“座椅式空间赋存形态明显。与已有研究成果对比发现,二者之间存在展布特征、展布位置、展布关系3方面的差异。
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出版历程
收稿日期:  2020-09-08
修回日期:  2021-08-20
刊出日期:  2021-08-20

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