吴忱, 张秀清, 马永红. 华北山地地貌面与新生代构造运动[J]. 华北地震科学, 1996, 14(4): 40-50.
引用本文: 吴忱, 张秀清, 马永红. 华北山地地貌面与新生代构造运动[J]. 华北地震科学, 1996, 14(4): 40-50.
Wu Chen, Zhang Xiuqing, Ma Yonghong. THE UPLAND MORPHOLOGIC SURFACE AND NEOZOIC TECTONIC MOVEMENT IN NORTH CHINA[J]. North China Earthquake Sciences, 1996, 14(4): 40-50.
Citation: Wu Chen, Zhang Xiuqing, Ma Yonghong. THE UPLAND MORPHOLOGIC SURFACE AND NEOZOIC TECTONIC MOVEMENT IN NORTH CHINA[J]. North China Earthquake Sciences, 1996, 14(4): 40-50.

华北山地地貌面与新生代构造运动

THE UPLAND MORPHOLOGIC SURFACE AND NEOZOIC TECTONIC MOVEMENT IN NORTH CHINA

  • 摘要: 华北山地有三期山地夷平面、四期河流阶地面。表明新生代地壳运动具有垂直差异性质。以上升运动为主,平均升幅1700m,速度0.031mm/a,以第四纪为最大。全区新生代地壳构造形迹可划分出3大类、8亚类和32个小类。在新生代构造运动中,又划分出第四纪以来的新构造运动和晚更新世以来的最新构造运动。

     

    Abstract: The North China upland has 3-stage upland planation suphaces and 4-stage river terrace suphaces. It is showed that the Neozoic crustal movement showed vertical difference characteristics. The movement is mainly uplift movement, with everage uplift amplitude being 1700m, rate 0.031mm/a, the largest one being in Quaternary period. The Neozoic crustal tectonic traces in the whole area can be divided into 3 large categories, 8 subcategories and 32 small categories. In the Neozoic tectonic movement, the Neozoic tectonic movement since Quaternary period and the Neozoic tectonic movement since Epleis-tocene have also been divided.

     

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