地球化学分散流异常找矿原理

Geochemical Prospecting Anomalies Dispersed Flow Principle

研究区位于华南板块二级构造单元扬子陆块南缘和华南褶皱带的交接部位。加里东造山运动期,该区处于华南褶皱带变形的前锋,地质条件复杂,所以地球化学探矿是非常适合的。通过了解区内金属矿成矿的有关构造、地球化学信息和矿产地质信息,根据分散流数据分析圈出异常靶区,确定矿化带,寻找矿体。

The study area is located in the South China plate tectonic units of the secondary transfer of the Yangtze craton and southern parts of the southern edge of the fold belt. Caledonian orogeny of the district in the South China fold belt deformation striker, complex geological conditions, so it is very suitable for geochemical prospecting. By understanding the regional metal mineralization related to structure, geochemical and mineral geological information, according to the data analysis circle dispersed flow anomaly targets, identified mineralized zones, looking for ore.