实验证实，岩块在高温高压受力变形后，其矿物中的元素将发生迁移和变化，在相同条件下，同一矿物中的不同元素或相同元素在不同矿物中具有不同的迁移和变化规律。实验结果说明，就许多内生金属矿床成矿作用而言，构造及构造变形不仅为成矿热液的运移、沉淀提供场所，而且在某种程度上能促使成矿元素的活化、分异甚至富集。 Experiments show that under the same conditions, the different elements or the same elements in the same mineral have different migration and variation rules in different minerals under the same conditions after the rock block undergoes deformation under high temperature and high pressure. The experimental results show that for many endogenic metallogenic mineralization, tectonic and tectonic deformation not only provide a place for migration and deposition of hydrothermal fluids, but also promote the activation and differentiation of ore-forming elements to a certain extent Even rich.