岩性和构造控制了南京汤山地区的地貌格局和碳酸盐岩山地岩溶地貌发育。
Lithological character and geologic structure determine the landform pattern and its evolution in Tangshan area, Nanjing.
广西岩溶地貌发育基本上均处于热带、亚热带环境中，为一较为典型的热带岩溶地貌。
The development of Guangxi karst geomorphology, with long geological history, was basically under tropical or subtropical environment, so it belongs to tropical karst geomorphology.
该文以岩溶地貌发育典型、碳酸盐岩出露面积广的贵州省为例，论述了岩溶区生态环境脆弱性类型划分的主要原则，探讨了脆弱性类型划分的指标并进行了量化。
With Guizhou karst areas as an example, this paper discusses the main principles and quantifies the index for division of eco-environmental fragility types in karst region.
这种时间上的差异，不仅造成了发育时气候上的差异，还造成了广西各地区热带岩溶地貌类型、形态上的不同。
The difference in time corresponded to the difference in climate, so there is difference in type and shape of Guangxi tropical karst geomorphology.
中国南方岩溶地区分布有面积广泛的碳酸盐岩，发育多种岩溶地貌。
The carbonate rock is widespread in South China where there are various karst topography.
中国岩溶地貌特别典型，洞穴堆积也十分发育，具有世界意义。
There is very developing karst and pultiple cave sediments in China.
中国岩溶地貌特别典型，洞穴堆积也十分发育，具有世界意义。
There is very developing karst and pultiple cave sediments in China.
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