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石人嶂钨矿是粤北钨矿化矿集区的一个中型的石英脉型钨矿床,垂向上具有典型的“五层楼”模式(韦龙明等,2008),区内岩浆活动频繁,在燕山期发生大规模成矿作用(覃日贤,2013),其中以燕山第二、第三期次的大规模侵入为主,在官坑、黄草地形成与钨矿化关系密切的莲花山隐伏花岗岩体,属燕山期复
The Shirenguan tungsten deposit is a medium-sized quartz vein tungsten deposit in the tungsten mineralized area in northern Guangdong Province and has a typical “five-story” vertical pattern (Wei Longming et al., 2008). Magmatic activity in the area is frequent, In the Yanshanian period, a large-scale mineralization occurred (Qin et al., 2013). The large-scale intrusion of the second and third stages of Yanshan dominated the formation of the Lianhuashan hiding granite, which is closely related to tungsten mineralization in Guankeng and Huangcao Body, is a complex Yanshan period