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Crystallization differentiation for granite is the main diagenesis mode.
结晶分异作用为花岗岩的主要成岩方式。
Look at the rock under your foot. This light red colored rock is called granite which is derived from the crystallization of molten magma.
你脚下的岩石,这种浅红色的岩石叫做花岗岩,它是由熔融的岩浆冷却结晶而形成。
Beside fractional crystallization model, liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
除了结晶分异模式外,富氟花岗岩浆液态不混溶作用也是伟晶岩成岩成矿的重要机制。
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