安徽淮南舜耕山位于华北克拉通淮南煤田南缘逆冲推覆构造带，天然出露与人工剥露地质遗迹数量众多，系统地查明地质遗迹资源类型、分布及特征可为区域地质对比研究以及地学科普与旅游规划工作奠定重要基础。文章通过野外地质调查，共发现舜耕山主要地质遗迹点62处，可划分为3大类、8类、14亚类，其中以华北型寒武系—奥陶系典型剖面、碳酸盐岩地貌、断裂构造以及矿业遗址等地质遗迹景观尤为发育，具有极高的科研和观赏价值；结合前人研究资料，初步讨论了舜耕山地质遗迹成因及其区域地质背景，为舜耕山地质遗迹资源开发提供理论依据；针对舜耕山在地质遗迹资源保护与开发利用存在的问题，提出对应的远景规划和建议。

The Shungeng Mountain in Huainan, Anhui Province, is tectonically located in the southern thrust-napped belt of the Huainan Coalfield within the North China Craton (NCC) and hosts many natural and artificial exhumed geoheritages. According to the field geological survey, 62 major geoheritage sites have been identified in the Shungeng Mountain, which can be divided into 3 major categories, 8 categories and 14 subcategories. Among them, typical Cambrian-Ordovician sections of the NCC, karst topography, fault structures and mining heritages are well developed and are of high scientific research and ornamental value. Based on the previous studies, the genesis and regional geological background of these geoheritages in the Shungeng Mountain are discussed, which provide a theoretical basis for the proper exploitation of the geoheritage resources. In light of the problems existing in the protection and exploitation of geoheritage resources in the Shungeng Mountain, this paper puts forward suggestions for long -term planning.