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根据某滑坡区地下水氢氧同位素组成测试成果，系统地研究了该区地下水的起源及形成机制．研究表明，该区地下水具有大气降水补给的特点，其同位素组成具有明显的温度效应和海拔效应，温泉与冷泉水的出露与区域高热流值和构造以及大气降水的补给量有着密切的关系．
According to the results of hydrogen and oxygen isotope composition test of groundwater in a landslide area, the origin and formation mechanism of groundwater in this area are systematically studied. The results show that the groundwater in this area has the characteristics of atmospheric precipitation recharge. Its isotopic composition has obvious temperature effect and altitude effect. The hot spring and cold spring water are closely related to the regional high heat flux value and structure as well as the recharge of atmospheric precipitation.