本文所称的地貌-地质环境,包括各个地质历史时期形成的碳酸盐岩在溶蚀及流水等因素的作用下塑造的地貌景观环境,以及形成可溶岩的古地理沉积相环境。前者主要指挽近地质时期以来,在新构造运动与流水、溶蚀等内外营力的综合作用下,对地壳表层改造所形成的地貌环境;后者则指形成可溶岩沉积物的古地理环境,因古地理沉积相的差异制约着物质 The so-called geomorphological-geologic environment, as referred to in this paper, includes the geomorphic landscapes formed by carbonate rocks under various geologic historical periods under the influence of erosion and flowing water, and the paleogeographic sedimentary facies forming soluble rocks. The former mainly refers to the geomorphic environment formed by the surface alteration of the crust under the combined effect of Neotectonic movement, flowing water, erosion and other external and internal forces since the recent geological period; the latter refers to the paleogeographic environment that forms the sediments of soluble rocks, Due to the difference of sedimentary facies in ancient geography, the material is restricted