新疆三塘湖盆地水文地质条件较为复杂,水文地质研究程度低。通过对控制地下水赋存及其富水性的机制进行分析,确定了控制盆地地下水的赋存及其富水性的主要因素有补给源、控水构造、地层厚度和地形地貌。盆地内地下水富集区均与控水构造活动密切相关,在盆地内非储水构造分布地段,地下水富水性较弱或无地下水赋存。 The hydrology and geology condition of Santanghu Basin in Xinjiang is rather complicated, and the degree of hydrogeology research is low. Through analyzing the mechanism of controlling groundwater storage and its water-richness, the main factors that control the occurrence and water-richness of groundwater in the basin are recharge source, water control structure, stratum thickness and topography. The groundwater-rich areas in the basin are closely related to the water control tectonic activities. In the non-storage structure distribution areas in the basin, the groundwater is weak or without groundwater.