文章分析了黄土高原地下水形成的地质环境 ,认为降水量、地形地貌、岩性构造和地下水循环是造成黄土高原严重缺水的主要因素 ,地层岩性和新构造运动是影响地下水富集的决定性因素。指出黄土高原基岩风化带潜水的相对富水岩组和富水地段 ,提出研究含水层的岩性和构造 ,寻找基岩风化带潜水是解决黄土高原局部地段缺水的较好途径。 This paper analyzes the geological environment of groundwater formation in the Loess Plateau. It is concluded that precipitation, topography, lithology structure and groundwater circulation are the main factors causing serious water shortage in the Loess Plateau. The stratigraphic lithology and neotectonic movement are the decisive factors affecting groundwater enrichment . It is pointed out that the relatively water-rich rocks and water-rich rocks in the weathered bed of weathered bedrock of the Loess Plateau suggest that it is a good way to study the lithology and structure of the aquifer and to find the weathered bed for diving in the weathered bed of the loess plateau.