The karst cave is a very important landscape and high grade traveling resource in the cone karst area.
锥状喀斯特是湿热带地区重要的喀斯特地貌景观类型和高品位的旅游资源。
The result can find whether the large area of Karst systems belong to the same vadose cave system, which provides the reliable geological data for the study of Karst leakage problems.
结果表明，该区地表水与地下水化学特征比较类似，为判定大区域内岩溶系统是否属于同一流动系统，解决岩溶渗漏问题提供了可靠的基础地质资料。
The research shows that the induced factors of karst collapse are the clay cap beds, the karst cave and the pumping of the groundwater in the area.
研究表明，覆盖粘土层、岩溶及人工疏降地下水，是该地区岩溶塌陷形成的基本条件。
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