摘要
岩溶地下河是云贵高原重要的岩溶形态,它不但分布广,而且地下水资源丰富,因此地下河已成为高原岩溶地下水研究的中心环节与主要供水水源。
Karst underground rivers are a major karst form of carbonate rock areas in Southern China and also a unique form for underground water to exist, so the study is of important significance and practical value.
The underground rivers in Yunnan-Guizhou Plateau are characterized by great numbers, complex types and large scales. According to statistics, there are more than 2000 underground rivers in the plateau area, of which there are 27 rivers whose discharges are more than 1.5m3/sec. These large underground rivers are mainly distributed in Eastern Yunnan and Western Guizhou.
The development of underground rivers in Yunnan-Guizhou Plateau is mainly influenced by the factors of lithology, structure, geomorphology and palaeokarst, etc., especially by the plateau geomorphologic action.
出处
《贵州地质》
1990年第2期105-113,共9页
Guizhou Geology
