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.
层析成像结果较好地揭示了地壳内部、尤其是浅部地壳的横向速度变化。短周期的群速度分布同地表地质结构、地形密切相关；
The maps at short periods reveal an evident lateral heterogeneity in the crust of North-China, quite well in agreement with known geological and tectonic features.
随着地表露头矿、浅部矿的减少，地质勘查的任务将更多地是寻找隐伏矿、深部矿及边远地区的矿产。
Concealed ores, deep buried ores and the resources of the border area will be searched more than ever before with the decrease of outcrop ores and shallow ores,.
随着地表露头矿、浅部矿的减少，地质勘查的任务将更多地是寻找隐伏矿、深部矿及边远地区的矿产。
Concealed ores, deep buried ores and the resources of the border area will be searched more than ever before with the decrease of outcrop ores and shallow ores,.
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