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断裂勾通深部气源和浅部储集层,是天然气垂向运移的主要通道。
They link deep gas sources to shallow reservoirs, and are main pathways for the vertical migration of natural gas.
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.
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