Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
除了
异模式外,富氟花岗
浆液态不混溶作用也是伟成成矿的重要机制。
Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
除了异模式外,富氟花岗浆液态不混溶作用也是伟成成矿的重要机制。
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