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海水经常被认为是地壳古火山岩铜、锌、铅成矿体系中质量和热传输的主要营力。在海底热液喷口地区存在着活跃的高温硫化物成矿现象,对这种现象进行研究,查明了海水在海洋环境中对贱金属、贵金属的溶解性,搬运及沉积过程中所起的作用。我们已经知道海洋中的这个过程是全球的地球
Seawater is often considered as the mainstay of mass and heat transport in the copper, zinc and lead ore-forming systems of ancient crustal volcanic rocks. There is an active phenomenon of high-temperature sulphide mineralization in the hydrothermal vents in the seabed. Studies on this phenomenon have identified the role played by seawater in dissolving, transporting and depositing base metals and noble metals in the marine environment . We already know that this process in the oceans is the earth on earth