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江西省境内,从地质学的范畴来说,基本上包括中国古陆台的江南地质和南岭准地糟地质区域内,属于比较古老而不大稳定的陆台。由于中生代三叠纪以至侏罗纪之末,白垔纪之初的造山运动所引起的岩浆活动,形成了许多具有瓷用原料独特性能的火成岩的风化产物。高岭土就是其中之一,它是这一成矿专属性的花岗正长岩在酸性介质与低温热液作用下,经风化、淋失后而残留的粘土质岩层高岭土
In the area of Jiangxi Province, from the perspective of geology, it basically belongs to the relatively old but not stable land station basically including the geologic areas of Jiangnan geology and Nanling quasi-terrain of China ancient landform. Due to the magmatic activity caused by the orogeny at the end of the Mesozoic and even the end of the Jurassic and the Early Cretaceous, many weathering products of igneous rocks with the unique properties of porcelain raw materials have been formed. Kaolin is one of them, which is the granite-bearing metamorphic granitic kaolinite that has been weathered and leached by acidic medium and low temperature hydrothermal fluids.