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南岭花岗岩成岩成矿类型划分的研究,在我国具有较长的历史.七十年代以来,比较深入和系统的从物质来源研究花岗岩的有:徐克勤教授等在论证花岗岩与成矿时,认为闽浙一带与偏中性岩石有关的部分钼铜铁矿属于深源产物;后来在第二届全国矿床会议(杭州)上,又较系统的从板块构造、岩石、矿物、地球化学等方面论证了两种成因系列花岗岩类与成矿的关系,提出了过渡地壳同熔型和陆壳改造型两种来源的花岗岩.1972年,中国科学院贵阳地球化学研究所和宜昌矿产地质研究所(即湖北地科所)从同位素
Nanling granite diagenesis and metallogenic classification of the study has a long history in our country.Since the seventies, more in-depth and systematic study of granite from the material sources are: Professor Xu Keqin argumentation granite and mineralization, that Part of Molybdenum-Cu-Fe deposits associated with the partial neutral rocks in the Fujian and Zhejiang regions belong to deep-sourced products. Later, at the Second National Conference on Deposits (Hangzhou), more systematical evidences from plate tectonics, rocks, minerals and geochemistry The relationship between the two genetic series of granitoids and mineralization was proposed and the transitional crust with the same type of melting and continental crustal reformation two sources of granite in 1972. Chinese Academy of Sciences Guiyang Institute of Geochemistry and Yichang Institute of Mineral Geology Geological Institute) from the isotope