本文论述了黑宝山山间盆地地下水的赋存条件及分布规律,该盆地沉积了一套中生代白垩系九峰山组碎屑岩、火山碎屑岩。岩石胶结较疏松,具有孔隙性、孔隙—裂隙性。为地下水的赋存提供了空间。并阐述了山间盆地地下水补给、迳流、排泄条件及地下水水化学特征。
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