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在系统统计湘南地区出露地层（震旦系至侏罗系）各类岩石成矿元素丰度（Ａ）、总体平均含量（Ｍ）、浓集克拉克值（Ｋ）和叠加强度参数（Ｍ／Ａ）基础上，结合湘南地区成矿特点，分析了Ｗ，Ｓｎ，Ｐｂ，Ｚｎ和Ｓｂ等元素的成矿作用．初步认为在湘南地区仅沉积作用、海底火山作用及热卤水作用难以形成上述元素的大型矿床，但通过沉积改造、热液叠加作用有可能形成层控型铅、锌矿床和锑矿床
The abundances of mineralization elements (A), the overall average content (M), the concentration of carats (K) and the superimposed intensity parameters (M / s) of various types of rocks in the exposed strata of Sinan to Jurassic, A), and combined with the characteristics of metallogenic deposits in southern Hunan, the metallogeny of elements such as W, Sn, Pb, Zn and Sb were analyzed. It is preliminarily believed that sedimentation, submarine volcanism and hot brine can not form large deposits of these elements in the southern part of Hunan Province. However, stratigraphic-controlled lead, zinc deposits and antimony deposits may be formed through sedimentary alteration and hydrothermal superposition