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通过对我国南方许多风化型高岭土矿床研究查明,在表生条件下形成高岭石-多水高岭石矿物的基本因素是决定于风化母岩的岩性和水介质的物化性质。水介质的物化性质又明显地受到风化母岩的岩性类型和结构构造、动力裂隙的发育程度、围岩的稳定性和透水性、气候、地形地貌和植被等因素的综合性制约。 我们把高岭石-多水高岭石视为具有相同结晶骨架和化学组份相似的一个演化系列
Through the study of many weathered kaolin deposits in the south of China, the basic factors for the formation of kaolinite-polyhydrated kaolinite minerals under supercritical conditions are determined by the lithology of weathered mother rocks and the physicochemical properties of aquifer media. The physico-chemical properties of the water medium are clearly constrained by the lithology type and structure of the weathered mother rock, the development of dynamic fissures, the stability and permeability of the surrounding rock, climate, topography, vegetation and other factors. We consider kaolinite-horsetail kaolinite as an evolutionary series that has the same crystalline framework and chemical composition