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二十年代初,我国翁文灏(1920)首先将与成矿有关的花岗岩类简单地划分为两种类型。即以长江中下游为代表与铁铜等有关的偏中性的一类,及以南岭为代表与钨锡等有关的偏酸性的另一类花岗岩,两者比较,前一类来自地下较深处,等等。其后,谢家荣(1936)曾分别称之为扬子式与香港式花岗岩类。自五十年代以来,我们(1958,1963)已开始认识到这种将与成矿有关的花岗岩类的二分
In the early 1920s, Wen Hao (1920) in our country first classified the granitoids related to metallogenesis into two types. Namely the middle and lower reaches of the Yangtze River as the representative of iron and copper and other related to the neutral one class and to the South Ridge and tungsten-tin and other related acidic and other types of granite, the two compared to the former one from the ground more Deep, and so on. Later, Xie Jiarong (1936) once called the Yangtze and Hong Kong-style granite classes. Since the 1950s, we (1958, 1963) have come to recognize that this dichotomy of the granitoids associated with metallogenesis