The silicon-rich mineralizing fluid process is a continuation of mineralization led by the mantle fluid metasomatism in crust.
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 research of ore-forming fluid includes large-scale translayer effect, mantle metallogenetic process, fluid thermodynamics and dynamics of fluid.
成矿流体的研究主要包括流体的广域穿层效应，地幔流体成矿作用，成矿流体热力学、动力学等几个方面。
The research of ore-forming fluid includes large-scale translayer effect, mantle metallogenetic process, fluid thermodynamics and dynamics of fluid.
成矿流体的研究主要包括流体的广域穿层效应，地幔流体成矿作用，成矿流体热力学、动力学等几个方面。
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