摘要
陇南市武都区历经长期多阶段复杂的地质构造演化。该区地质遗迹的发育与大地构造分区特征紧密贴合,不同的构造分区孕育了不同的地质遗迹类型,主要表现在峡谷地貌、峰林地貌以及部分水体景观等地质遗迹的分布上,这些景观在构造运动非常强烈的地区,尤其是水平运动极为活跃的地区,会有明显的发育。
Wudu District of Longnan City has undergone a long-term,multi-stage and complex geological tectonic evolution.The development of geological relics in this area is closely related to the characteristics of geotectonic partitions.Different geotectonic partitions have produced different types of geological relics,which are mainly reflected in the distribution of geological relics such as valley geomorphology,kegel andturm karst geomorphology,and some water body landscapes.These landscapes are significantly developed in areas with strong tectonic movements,especially in areas with extremely active horizontal movements.
作者
薛文灏
冯丽娟
XUE Wenhao;FENG Lijuan(Geological Mineral Exploration and Development Research Institute of Gansu Nonferrous Metals Geological Exploration Bureau,Lanzhou 730000,Gansu,China;The Second Geology and Mineral Exploration Institute of Gansu Provincial Bureau of Geology and Mineral Exploration and Development,Lanzhou 730000,Gansu,China)
出处
《资源信息与工程》
2025年第2期30-34,共5页
Resource Information and Engineering
关键词
陇南市武都区
地质遗迹
地质构造
Wudu District,Longnan City
geological relics
geological tectonic
