摘要
青藏高原多年冻土区的地下水是高原特定的地质地理环境下的产物,多年冻土的存在控制地下水的形成和分布,新构造运动是影响区域水文地质条件的主导因素,地下水和多年冻土相互作用、相互制约,导致区域水文地质条件复杂化。
The groundwater of permafrost area of Qing-Zang plateau is produced under thespecial geologic-geographic environment of the plateau. Permafrost controls the origin and distri-bution of groundwater and new tectonic movement is the main factor to affect the regional hydro-geolgical condition. Since the interaction and interrestriction bet ween groundwater and per-mafrost,the regional hydrogeo logical conditon become complex.
关键词
青藏高原
多年冻土区
地下水
水文地质
Qing-Zang plateu
Permafrost area
Groundwater
Hydrogeological characteristics
