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成矿溶液的多样性与多来源性,已得到普遍地承认.本文讨论的对象是壳源重熔花岗岩浆期后热液充填构造裂隙所形成的脉钨矿床. 自1847年法国人埃利·德·鲍蒙奠定了岩浆热液成矿说的基础以来,许多学者对矿质在热液中的搬运-沉淀过程做了大量研究工作,但多半只注重矿质在热液中搬运一沉淀形式的研究,而忽视了成矿物质运动的另一方面——携带矿质的溶液的流动状态.即使是对热液中矿质的搬运形式和沉淀方式,在认识上也仍有较大的争论.本文根据华南脉钨矿床的大量实际材料,粗略讨论以下几个问题.
The diversity and multi-origin of ore-forming solutions have been widely acknowledged.The object of this paper is the vein-tungsten deposit formed by hydrothermal fissure tectonic fractures after the reformation of crustal refractile granites.From 1847, the French Eli Since de Baumng laid the foundation for the magmatic hydrothermal mineralization, many scholars have done a lot of research on the transport-precipitation process of minerals in hydrothermal fluids, but most of them focus only on the research on the transport of a precipitate in the hydrothermal fluids , While ignoring the other side of the movement of ore-forming material - the flow of the solution carrying minerals.While there is still a great debate on the transport modes and deposition methods of minerals in hydrothermal fluids, A lot of tungsten material in the actual material, a rough discussion of the following questions.