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南岭地区块状硫化物矿床与下扬子地区块状硫化物矿床均产生在大陆地壳背景上的断裂拗陷带中，主要形成于泥盆纪、石炭纪。本文通过对上述两地欧块状硫化物矿床的矿床类型、矿床共生组合特征、伴生组份、产出特征、基底成份和性质，沉积大地构造环境、成矿温度、盐度、溶液成份、同位素组成特征以及成矿物质来源等的综合对比，认识到南岭和下扬子地区块状硫化矿床在所有以上方面均存在明显不同，从而将南岭和下扬子区块状硫化物矿床分别命名为＂南岭式＂＂下扬子式＂，并探讨了它们与地壳演化的关系。
Both the massive sulfide deposits in the Nanling area and the massive sulfide deposits in the Lower Yangtze region are produced in the fault-depression zone on the continental crust background and are mainly formed in the Devonian and Carboniferous. Based on the types of the deposits, the symbiotic assemblages, the associated components, the output characteristics, the composition and properties of the basement, the tectonic setting of the tectonic environment, the temperature of the ore-forming, the salinity, the solution composition, the isotopes Compositional characteristics and sources of metallogenic materials, we know that the massive sulphide ore deposits in the Nanling and the Lower Yangtze are obviously different in all the above aspects, so that the massive sulphide deposits in the Nanling and the Lower Yangtze are respectively named “ Nanling style ”and“ Yangtze style ”, and explored their relationship with the evolution of the crust.