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通过与美国Fortknox等7个大型金矿床[1]及广东莲花山斑岩型含金钨矿床的对比,认为龙潭现存铁帽状钨矿相当于含钨(锡)氧化物的硫化物带的中上部,其中下部主体硫化物带应是今后找金评价的重点。
By comparing with the seven large gold deposits [1] such as Fortknox in the United States and the Lianhuashan porphyry-type gold-bearing tungsten deposit in Guangdong Province, it is considered that the existing iron-capped tungsten ore in Longtan is equivalent to the sulfide belt containing tungsten (tin) oxide Upper, of which the lower part of the main sulfide belt should be the future focus of gold evaluation.