结果表明，本区地下水有三个来源：深部喀斯特岩溶水、浅部孔隙水和地表水。
These results show that the underground water has three sources, namely deep karst, shallow porous and surface waters.
岩溶地下水赋存于地表以下浅部岩溶带、构造控制的中部岩溶带和深部古溶蚀带。
The karst groundwater stores in the shallow karst zones below the surface, the middle karst zones controlled by geological structures and the deep zones of fossil karst.
我国目前大多数地表浅部矿床(矿体)已被探明、开采，寻找深部隐伏矿体已成为当务之急。
With most of the surface (shallow) ore deposits (ore bodies) in China being demonstrated and exploited, the future targets will be aimed at the concealed ore bodies at depth.
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