溶蚀火山角砾岩,气孔玄武岩和裂缝发育的致密玄武岩是区内最好的储集岩类。
The best reservoir rocks in the area are dissolution volcanic breccias, vesicular basalt and tight basalts with developed fractures.
这样就造成了主要沿水流方向发育的溶蚀通道。
This produces solution channels that develop mainly in the direction of the flow.
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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