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福建行洛坑钨(钼)矿床的成因类型,至今众说纷云。概括起来,有如下几种观点:岩浆期后高温热液充填型(原矿区有关地质报告,1963—1966);花岗岩细脉浸染型(谢家荣,1964);变花岗岩型(林运淮,1979);从各种不同角度称之的斑岩型(莫柱荪,1975;谭运金,1979;刘文章,1981……);此外,还有认为属于与花岗岩有关的脉状钨矿等等。目前争论的焦点是,行洛坑钨矿究竟属于重熔地壳型(陆壳改造型)花岗岩钨矿成矿系列矿床,还是属于与火山岩、次火山岩有关的斑岩矿床。探讨这一问题,不仅具有成矿理论上的
Fujian Xing Luo Hang tungsten (molybdenum) deposits of genetic types, so far said numerous. To sum up, there are several views as follows: high-temperature hydrothermal filling type after the magmatic period (geological reports of the original mining area, 1963-1966); granite vein disseminated type (Xie Jialong 1964); granite type (Lin Yun-huai 1979) Various types of porphyry types are known from the different perspectives (Mo Kusun, 1975; Tan Yunjin, 1979; Liu Wenzhang, 1981 ...); in addition, there are also thought to belong to granite related vein tungsten and so on. At present, the focus of debate is whether the Xinglongkeng tungsten deposit belongs to the remelted crust type (continental crust alteration type) granite tungsten mineralization series deposit or belongs to the porphyry deposit related to volcanic rocks and subvolcanic rocks. To explore this issue, not only has the theory of mineralization