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南岭是全国乃至全世界上钨、锡、钼、铋等多金属矿产资源最丰富的地区,这些金属成矿作用与花岗岩有着密切的关系。众所周知,燕山期花岗岩与南岭地区大规模成矿作用有密切关系,因此相关方面的研究较深入,且成果很多。而对印支期、加里东期花岗岩成矿则探讨不多(华仁民等,2013);同样,在研究区域上,以往大多关注南岭东段与中段,而对于加里东期和印支期花岗岩出露较多的南岭西段的研究则显得很不
Nanling is the most abundant polymetallic mineral resource such as tungsten, tin, molybdenum and bismuth in China and even in the world. The mineralization of these metals is closely related to granite. As we all know, Yanshanian granite and Nanling area are closely related to the large-scale mineralization, so the relevant aspects of research are more in-depth, and the results are many. For the Indosinian period, the Caledonian granitoids mineralization is not discussed (Huaren et al., 2013). Similarly, in the study area, most of the past focuses on the eastern section and middle section of Nanling. For the Caledonian and Indo-China The study of the granites in the Nanling west section is not very clear