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位于华南褶皱系东部政和—大浦北东向断裂带内梅仙矿田西部的丁家山铅锌矿床,先后被认为是接触交代型矿床(闽西地质队,1977;石得凤等,2012;石得凤,2012)、SEDEX型和VMS型矿床(徐克勤等,1996)等。本文通过赋矿层位地层的矿体分布特征、矿化特征、蚀变类型等的对比,浅
The Dingjiashan Pb-Zn deposit, located in the western part of Zhengxianhe-Dapu north-east fault zone of South China fold system, has been considered to be a contact metasomatic deposit (Geology Team of Minxi Basin, 1977; Shi Defeng et al., 2012; Defeng, 2012), SEDEX and VMS deposits (Xu Keqin et al., 1996). Based on the comparison of ore body distribution characteristics, mineralization characteristics, alteration types and so on,