摘要
根据贵州省的地质特征和地下热矿水的形成条件及水文地质地球化学特征，将贵州的地下热矿水分为受深断裂控制的深循环型中、低温热矿水和沉积盆地深埋型中、低温地下热卤水两个基本类型。
According to the geological setting,the controls on the formation of mineral wotar and its hydrogeochemisfry, the thermal mineral water can be classfied as two types, i. e. deep cyolic meso-hypo-temperature thermal water controlled by deep fracture and mesohypotemperature hot bine buried deeply in dipositional basins.
出处
《贵州地质》
1994年第4期330-333,共4页
Guizhou Geology
