These characteristics indicate that the ore-forming fluid resulted from fractional crystallization of magma, with the participation of some connate water at the late stage.

  • 根据这些特征可推断出成矿流体源于花岗岩浆的结晶分异,晚期有少量建造水混入。

  • 互联网摘选 2025-01-20 11:38:14

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