Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
除了结晶分异式外,富氟花岗岩浆液态不混溶作用也是伟晶岩
岩
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.
除了结晶分异式外,富氟花岗岩浆液态不混溶作用也是伟晶岩
岩
矿的重要机制。
The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.
矿床类型以岩浆晚期分异交代型、液型、伟晶岩型、风化壳型和砂矿型为主。
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