该文从时空关系、微量元素特征、稀土元素特征等方面对郴州市枞树板地区铅锌（银）矿化与花岗斑岩脉的关系进行了阐述，指出铅锌（银）成矿作用与花岗斑岩脉在成因上关系不大，而与燕山早期花岗岩（千里山岩体）有关，成矿物质主要来源于燕山早期花岗岩，成矿时代为燕山早期，成矿早于花岗斑岩脉的侵位，两者的共生关系是受同一组断裂控制的。 This paper describes the relationship between lead-zinc (silver) mineralization and granite-porphyry veins in Fushulin area in Chenzhou from the aspects of spatio-temporal relationship, trace element characteristics and rare earth element characteristics. It is pointed out that the lead- It is related to the genesis of the granite porphyry veins but not to the Yanshanian early granite (the Qianlishan granite). The metallogenic materials are mainly derived from the early Yanshan granites, the metallogenic epoch is the early Yanshanian, and the mineralization earlier than granite The emplacement of dikes, the symbiotic relationship between the two is controlled by the same group of faults.