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 fluid transported as isothermal process under a particularly ore forming environment.
由于其特殊的成矿环境，流体的输运过程是一种近于等温的过程。
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