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.
文中给出了该区P波反射法探测基岩界面、溶洞、断层和溶蚀带分布的应用实例。
A case history of the application of the P-wave reflection method in that area to investigate the bedding plane of bedrock, karst cave, fault and the distribution of the dissolution belt is given.
滨海岩溶具有与内陆一般岩溶区不同的发育机理，其过渡带混合溶蚀作用是控制滨海岩溶发育的最主要因素之一。
The development mechanism of littoral karst differs from inland karst, and the mixture corrosion effect is one of the most important factors which control the development of littoral karst.
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