ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    甘肃内蒙古北山地区构造单元划分

    The division of tectonic units of Beishan area, Gansu-Inner Mongolia

    • 摘要: 北山地区构造单元归属历来为众多地质学家所关注。笔者结合区内的地质实际,拟定出一、二、三级构造单元划分和命名的一般原则;运用板块构造观点和多旋回开合构造理论,将本区共划分出3个一级构造单元,8个二级构造单元和26个三级构造单元;阐述了各构造单元主要地质特征。认为本区先后存在红柳河—牛圈子—洗肠井(早古生代)和红石山—百合山—蓬勃山(晚古生代)两条缝合带,后者是哈萨克斯坦与塔里木板块的最终缝合带

       

      Abstract: This paper gives some general principles about the division and naming of tectonic units of Beishan area. According to the theory of plate tectonics and polycyclic opening-closing tectonics,Beishan area is divided in to three first-order tectonic units,eight second-order tectonic units and twenty-six third-order tectonic units. There are two suture zones in Beis-han area:the Hongliuhe-Niujuanzi-Xichangjing suture zone(Early Paleozoicera)and the Hongshishan-Pengboshan suture zone(Upper Paleozoic era),and the latter is the final plate junction between the Tarim Plate and Kazakh stan Plate.

       

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