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地球化学分散晕的形成问题在研究复杂的地质体系时具有重大的理论意义。因此,研究在含金砂矿上的现代水系中形成的金的岩石地球化学和水文地球化学分散晕的结构也有很大的理论和实际意义。到目前为止,金在河道水流条件下的许多搬运和迁移的形式问题仍是有争议的问题,这一问题的解决就更为重要。例如波格列勃尼亚克等人在普里巴米耶用水文地球化学方法研究金矿点的普查前景时确认:“自然砂金不能明显地转入水溶液,因此现有的砂金矿不会形成水分散流”。同时,已有四十多年历史的水文地球化学
The formation of geochemical dispersion halo is of great theoretical significance in the study of complex geological systems. Therefore, it is of great theoretical and practical significance to study the geochemistry of gold formed by the modern water system on gold-bearing sands and the hydrogeochemical dispersion halo. So far, the issue of the form of many movements and relocations of gold under river water flow conditions remains a matter of debate, and the solution to this problem is even more important. For example, Pogleboni et al., In the Primumyah study of census prospects of gold deposits using hydrogeochemistry, confirmed that “natural gold can not be apparently transferred into an aqueous solution and therefore the existing placer gold does not Form a water dispersion flow ”. At the same time, more than 40 years of history of hydrogeochemistry