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通过对贵州、广西亚热带岩溶地区碳酸盐岩红色风化壳典型剖面的矿物学与微结构研究 ,从不同研究尺度和剖面不同部位都观察到大量碳酸盐岩风化成土过程中交代作用发育的最直接和最重要的矿物与微结构证据。首次较为系统讨论了碳酸盐岩风化成土的交代作用机理 ,提出了碳酸盐岩风化成土过程中的矿物交代演化序列
Through the study of the mineralogical and microstructure of the typical carbonate red weathering crusts in the subtropical karst area of Guizhou and Guangxi Provinces, a great deal of carbonate rock weathering and earth-forming processes were observed from different research scales and different parts of the profile. The most direct and important mineral and microstructure evidence. For the first time, the mechanism of metasomatism of carbonate weathering into soil was systematically discussed, and the sequence of mineral metasomatic evolution during carbonate weathering