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通过３７次成岩实验研究认为：（１）在地壳温度下，地壳物质的重熔不可能形成石英闪长质或更基性的岩浆；（２）碱性玄武岩浆同化花岗质地壳，可以生成石英闪长质和花岗闪长质岩浆，所产生的岩浆高钾富碱，属高钾岩系，与铜陵地区侵入岩相似；（３）高压下形成的岩浆比中压下形成的岩浆更高钾富碱；（４）在岩浆演化过程中铜与钾似无成因联系，钾与铜的“相关性”与它们的趋同性有关，即两者均于岩浆晚期富集。
Based on 37 diagenetic experiments, it is considered that: (1) Crustal metamorphism can not be formed by remelting of crustal materials at crustal temperature; (2) Basaltic basalt magmas assimilate granitic crust to form Quartz diorite and granodiorite magma, the magma generated by high potassium and alkali, is a high-potassium rock series, similar to the Tongling intrusive rocks; (3) the formation of high pressure magma than the formation of magma more (4) There is no causative relationship between copper and potassium during magmatic evolution, and the “relativity” between potassium and copper is related to their convergence, that is, both are enriched in late magma.