On this basis, combining the distribution feature of sulfide in mantle and the model of mantlediapir uprising, the model of formation and evolution of second stage magma has been advanced.
在此基础上,结合地幔中硫化物的分布特点和地幔岩块底辟上升模式,提出了第二侵入期岩浆的形成演化模式。
2
Some times in the process there was reworking of diapir of mantle-sourced magma on the crust or lithosphere.