摘要
应用地表标志带和隐伏花岗岩进行隐伏、半隐伏石英脉型黑钨矿床预测和评价,必须研究其地质地球化学类型,只有属于钨锡硫化物型的标志带,才具有找矿评价意义。对隐伏花岗岩体预测研究,不仅要研究隐伏岩体的地球化学类型,还应研究岩体多期多阶段的成岩成矿作用,才具有找矿评价意义。
The use of the surface indication zone and hidden granite body to the prospecting forecast and evaluate the hidden and semi-hidden quartz-vein type wolframite deposit is studied. This paper studies the geological and geochemical features exhibited in the deposit geochemical type. Only under the condition that the deposit- geochemical type of surface indication zone belongs to wolfram-tin sulphide one, it can be suggested as a hidden or semi-hidden quartz-vein type wolframite deposits.
出处
《中国钨业》
CAS
北大核心
2008年第4期5-7,共3页
China Tungsten Industry
关键词
石英脉型黑钨矿
地表标志带
隐伏花岗岩
找矿评价
quartz-vein type wolframite deposits
surface indication zone
hidden granite body
prospecting evaluation
