On this basis, combining the distribution feature of sulfide in mantle and the model of mantle diapir 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。
Some times in the process there was reworking of diapir of mantle-sourced magma on the crust or lithosphere.
在某些地质时期还与幔源岩浆的底垫对地壳或岩石圈的改造有关。
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