流体成矿系统内具有一些重要特征，如各种地质要素的方向性、相关性和指示性变化。
There are several major characters such as the directive, relative and indicative changes of various geological features within a fluid ore forming system.
深部流体（ 地幔流体）及其成岩成矿作用的研究是当今地质科学研究的前沿领域，最近几年这方面的研究进展较快。
The researches on mantle_derived fluids in relation to ore_forming and oil_forming processes constitute one of the forefront fields in the earth science.
对产在五朵山花岗岩中的矿床（点）的地质背景、矿床特征、成矿流体及矿床成因等方面作了系统的研究。
The geological setting, deposit features, metallogenetic fluid and the genesis of the gold deposit hosted in the Wuduoshan granite were systematically discussed.
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