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通过不同温度和压力下岩块受力变形的模拟实验，证实了岩块受力变形导致成矿元素的迁移和富集，发现了高温高压下不同元素在同一温压条件下和同一元素在不同温压条件下具有不同的迁移和富集规律。实验表明，构造应力对许多内生金属矿产的形成、矿产中成矿元素的分带现象等都具有十分重要的作用。
Through the simulation experiments of rock mass deformation under different temperature and pressure, the deformation and deformation of rock mass led to the migration and enrichment of ore-forming elements. It was found that under the same temperature and pressure, Temperature and pressure conditions have different migration and enrichment laws. Experiments show that tectonic stress plays a very important role in the formation of many endogenous metallic minerals and the zonation of ore-forming elements.