地质异常成矿理论在多本沟地区铀成矿预测中的应用

Application of geologic anomaly metallogenic theory to uranium metallogenic prediction in Duobengou area

多本沟地区位于华北地台北缘内蒙地轴之内,已发现多个铀矿点、异常点。运用地质异常成矿理论分析研究区地质体时空异常特征与铀矿化的关系,认为研究区处于地质体时空异常叠加的部位,具有深部找矿潜力。

Duobengou area is located in Inner Mongolia geo-axis at the northern margin of North China Platform. Many uranium occurrences and anomalies have been found in this area. Geologic anomaly metallogenie theory is used to analyze the spatial-temporal relationship between the anomaly of geological bodies and uranium mineralization in this area. It is considered that the superimposed parts of anomalies of geological bodies with different spatial and temporal features possess uranium mineralization potential at depth.