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地球内部流体的活动乃是形成各种矿床的必要条件,是导致矿物聚积和金属成矿作用的前提。随着地球科学的进展,作为地球内部流休的重要组成部分,地幔流体受到越来越多的重视。众多学者就对世界首例白云郑博地幔流体交代稀土矿床的基础上,初步总结了地幔流休与成矿作用的基本问题。最新的研究资料证实,内蒙白云鄂博稀土矿是一个国内外罕见的地幔流体交代矿床;新疆尉犁县且旦布拉克超大型蛙石矿则是地幔流体交代成因的非金属矿床;出澳大利亚南部的Roxby Down(奥林
Fluid activity within the Earth is a necessary condition for the formation of various deposits and is a prerequisite for mineral accumulation and metallogenesis. With the progress of earth science, mantle fluid has drawn more and more attention as an important part of the earth’s internal circulation. Based on the first Baiyun Baiyun Zhengtang mantle fluid account for rare earth deposits, many scholars initially summarized the basic problems of the runoff and mineralization of mantle. The latest research data confirm that Inner Mongolia Bayan Obo Rare Earth Mine is a rare mantle fluid interchange deposit at home and abroad; Xinjiang Yuli County and Dan Burak super large frog quarry is a non-metallic mineral deposit of mantle fluid metasomatism; out of Roxby Down (Olin