释文：地下水盆地是承压水盆地和潜水盆地的总称。
以不同的研究尺度，白垩系地下水盆地可以划分为若干地下水流系统。
According to different dimensions, the cretaceous groundwater basin can be divided into many groundwater flow systems.
他补充说，地下水对海平面上升的作用将可能减少，因为随着地下水盆地的枯竭，将不会有多少水通过雨云进入到海洋中。
Groundwater's contribution to sea-level rise will probably diminish, he added, because as groundwater basins are depleted, there won't be as much water left to send through rain clouds to the oceans.
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