论文部分内容阅读
乌溪金矿位于安徽省泾县榔桥镇,是长江中下游多金属成矿带上新发现的成矿类型,是该区金矿找矿工作的新突破。矿体赋存于志留系上统举坑组碎屑岩中,侵入岩为一隐伏花岗斑岩—二长斑岩,主要受断裂构造控制。通过对矿区物化探异常特征的评价,对矿床成矿特征以及金资源储量做了详细预测,因此掌握了乌溪矿区物化探异常分布特征、矿床控矿因素及控矿规律、矿脉的分布特征、矿体赋存特征,该区显示出良好的资源远景和潜力。前人在乌
Located in Qiaqiao Town, Jing County, Anhui Province, Wu Xi Gold Mine is a newly discovered metallogenic type discovered on the polymetallic metallogenic belt in the middle and lower reaches of the Yangtze River and is a new breakthrough in gold prospecting in the area. Ore bodies occur in the Silurian clastic rocks in the Upper Silurian of Silurian. The intrusive rocks are a concealed granite porphyry-biPorphic porphyry and are mainly controlled by fault structures. Through the evaluation of the geophysical and geochemical anomalies in the mines, the ore-forming characteristics and reserves of gold resources have been predicted in detail. Therefore, the anomalous geophysical and geochemical distributions, the ore-controlling factors and ore-controlling rules, the distribution characteristics of the veins, Ore body characteristics, the area shows a good resource prospects and potential. Predecessors in Ukraine