历史的剖析在寻找金属的早期,找矿者很快便擅长通过基岩和地表环境特征来查明矿床.河流沉积物中的岩石和矿物碎屑使早期找矿者可以从那一连串的分散物追溯到基岩源头.最早期找矿者和现代勘查地球化学工作者之间的主要差异在于,找矿者运用了矿物调查,而地球化学工作者则使用化学分析. 在30年代,苏联和斯堪的纳维亚的工作者首先使用现代地球化学方法.发射光谱这种当时微 Historical analysis Early in the search for metals, the prospectors were quick at identifying deposits by bedrock and surface-environmental characteristics.The rock and mineral debris in the river sediments enabled early prospectors to find out from that succession of dispersions Dating back to the source of bedrock, the main difference between the earliest prospectors and modern prospecting geochemists lies in the fact that the prospectors used a mineral survey and the geochemical workers used the chemical analysis.In the 1930s, Scandinavian workers first used modern geochemical methods. Emission spectra of this time micro