梁收运, 刘高, 韩文峰. 2002: 黑山峡出口段中卫一同心断裂带结构特征. 工程地质学报, 10(S1): 72-76,90.
    引用本文: 梁收运, 刘高, 韩文峰. 2002: 黑山峡出口段中卫一同心断裂带结构特征. 工程地质学报, 10(S1): 72-76,90.
    LIANG Shouyun, LIU Gao, HAN Wenfeng. 2002: THE CHARACTERISTICS OF STRUCTURE OF ZHONGWEI-TONGXIN FAULT IN OUTLET OF HEISHAN GORGE. JOURNAL OF ENGINEERING GEOLOGY, 10(S1): 72-76,90.
    Citation: LIANG Shouyun, LIU Gao, HAN Wenfeng. 2002: THE CHARACTERISTICS OF STRUCTURE OF ZHONGWEI-TONGXIN FAULT IN OUTLET OF HEISHAN GORGE. JOURNAL OF ENGINEERING GEOLOGY, 10(S1): 72-76,90.

    黑山峡出口段中卫一同心断裂带结构特征

    THE CHARACTERISTICS OF STRUCTURE OF ZHONGWEI-TONGXIN FAULT IN OUTLET OF HEISHAN GORGE

    • 摘要: 在详实的野外调查和多种物探测试工作的基础上,辅以航卫片解译,对黑山峡出口段中卫一同心断裂带的平面与剖面结构特征进行了研究,结果表明:该区域中卫一同心断裂带从南向北主要由近东西向展布的F1~F3、F8(7)、F201和F2026条断层组成,平面上相邻断层间多处交会或重合并最终交于F201断层,剖面上除F3外,其余均向南倾,形成复杂的逆冲推覆迭瓦状活动构造带.

       

      Abstract: Based mainly on detailed field geological investigation and a few geophysical surveys while utilizing interpretation of aerial photograph and satellite picture subsidiary, the plane and profile structures of Zhongwei-Tongxin fault zone in the outlet of the Heishan gorge on the Yellow river are studied and hence some results are gained. The Zhongwei-Tongxin fault zone comprises of six secondary faults that are F1,F2,F3,F8(7),F201 and F202 from south to north and strike to east nearly. As for plane structure, the ends of each fault converge at the adjacent one among them and then overlap each other. All faults converge on fault F201.These faults with exception of F3 dip. to south and form a complex active imbricated shrusting nappe.

       

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