金属矿床的水文地球化学找矿方法,在褶皱区,特别是花寻找隐伏矿化时,可以得到最好的效果。褶皱区金属矿床的水文地球化学晕和分散流具有相当大的规模、多变的成分和很高的衬度。其形成在很大程度上取决于地质构造和景观条件。可分出三组具不同的分散晕和分散流形成条件的地区:气候潮湿并且没有永冻土的地区,气候干旱的地区,永冻土广泛分布的地区。在上述每一组地区进行水文地球化学找矿时都有一些不同的特点。迳流的强烈活动性,特别是在山区,决定了水、水文地球化学分散晕及分散流的化学成分也有较大的变化。因此,把晕和分散流划分 The metallogenic hydrogeochemical prospecting method, in the fold area, especially for flowers to find hidden mineralization, you can get the best results. Hydrographic geochemistry of the fold zone metallogenetic halo and dispersed flow has a considerable size, varied composition and high contrast. Its formation largely depends on the geological structure and landscape conditions. Three separate sets of zones with different conditions for dispersal of halo and dispersed flow can be distinguished: areas that are humid and have no permafrost, areas with arid climates and areas where permafrost is widely distributed. There are a number of different characteristics of hydrogeochemical prospecting in each of these areas. The strong activity of tidal currents, especially in mountainous areas, has also determined that the chemical composition of water, hydrogeochemical dispersion haloids and dispersed flows also vary considerably. Therefore, the dizzy and dispersed flow