在对平茶、肖家金矿进行流体包裹体同位素测年的基础上，结合最新的一批测年数据，认为雪峰地区金成矿带的成矿时代并非传统认识中的武陵—雪峰期（１０００Ｍａ～８０００Ｍａ），而是形成于加里东早期以后；加里东、印支—燕山期是雪峰地区两个主要的金成矿期，特别是印支—燕山期地台活化对该区大型金矿的形成起着重要作用。在此基础上，对当前流行的一些观点进行了初步探讨。 Based on the isotope dating of fluid inclusions in Ping tea and Xiaojia gold mine and the latest batch of dating data, it is concluded that the metallogenic epoch of the gold mineralization belt in Xuefeng area is not the traditional Wuling-Xuefeng period (1000Ma ~ 8000Ma), but formed after the early Caledonian; Caledonian, Indosinian-Yanshanian are the two major gold mineralization stages in Xuefeng area, especially the Indosinian-Yanshanian platform activation of the large gold The formation of mines plays an important role. On this basis, some prevalent views are discussed tentatively.