贵州盘县呼都金矿区成矿地质特征及找矿前景

Hudu District Gold Metallogenic Geological Characteristics and Prospecting in Guizhou Panxian

贵州盘县呼都金矿区是该区继砂锅厂、羊禾地、小尖山金矿发现之后的又一凝灰岩金成矿潜力区,通过已开展的1∶5万土壤化探测量,显示金土壤化探异常较好,针对两处金重点异常区实施地表浅部山地工程和少量钻探工程异常查证,结果显示车家槽子-猴耳包一带和哈树头-田坝头-闭塞一带金矿地表蚀变情况较好,硅化较强烈,推测其深部具有良好的找矿前景。

Guizhou Panxian Hudu gold district is the region of tuff gold metallogenic potential areas following the Panxian Shaguochang, Yanghedi, Xiaojianshan gold. Through the 1：5 million soil has been carried out in geo- chemical survey, revealing soil geochemical anomaly is fine, According to the two key gold anomalies, carry on the surface of shallow mountain project and a small amount of drilling engineering abnormal verification, results show that the Chejiacaozi-Houerbao and the Hashutou-Tianbatou-Bisai area gold surface alteration situation bet- ter, is strongly silicified, speculated that the deep has good ore prospects.