陇南市武都区地质遗迹分布、形成及演变规律研究  

STUDY ON THE DISTRIBUTION,FORMATION AND EVOLUTION PATTERN OF GEOLOGICAL RELICS IN WUDU DISTRICT,LONGNAN CITY

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)

机构地区：[1]甘肃省有色金属地质勘查局地质矿产勘查开发研究院,甘肃兰州730000 [2]甘肃省地质矿产勘查开发局第二地质矿产勘查院,甘肃兰州730000

出　　处：《资源信息与工程》2025年第2期30-34,共5页Resource Information and Engineering

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.

关 键 词：陇南市武都区 地质遗迹 地质构造 

分 类 号：P942[天文地球—自然地理学]