因此，富硅成矿流体作用实质上是地幔流体交代作用在地壳内成矿作用中的延续。

The silicon-rich mineralizing fluid process is a continuation of mineralization led by the mantle fluid metasomatism in crust.

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因此，富硅成矿流体作用实质上是地幔流体交代作用在地壳内成矿作用中的延续。

The silicon-rich mineralizing fluid process is a continuation of mineralization led by the mantle fluid metasomatism in crust.

youdao