The Louli gold deposit is located on the northern side of Hongshan alkalic complex, and the host rock of the orebody is the volcanic tufa. This is the first ore deposit of such type found in volcanic tufa in the southern segment of the Taihang Mountain, and its metallogenic regularity and deep metallogenic prospect evaluation are of guiding significance for delineating potential prospective areas and increasing mineral resources. Based on the regional mineralization regularity and geological characteristics, the authors systematically collected rock samples in 2 drill holes, and used Gregorians zonality index method and generalized contrast value method to compute and determine vertical zoning sequence of indicator elements. The results show that different calculation methods may produce somewhat different element orders, but the active stages of hydrothermal fluid and spatial superposition mode of halos are identical. The computed result of two drill holes shows the obvious coexistence of frontal halo and tail halo and axial zoning characteristics. The active process of hydrothermal fluid was analyzed based on the trace elements geochemical parameter axial variation. The results obtained show that the vertical zoning of two drill holes are made up of two stage hydrothermal circulation, suggesting that the formation of gold deposit is of multi-stage characteristics.%娄里金矿位于邯郸洪山杂岩体北侧的火山凝灰岩中。该类型金矿在太行山南段为首次发现，其成矿规律和深部成矿潜力的研究对圈定成矿远景区及增加矿山资源量有重要的指导意义。据此系统采集了矿区ZK11-2和ZK16-1钻孔岩心样品，在分析区域成矿地质规律和矿床地质特征的基础上，采用格里戈良分带指数法和广义衬值法两种方法计算了元素垂向分带序列，结果显示不同方法虽在元素排列顺序上存在一定差异，但在反映热夜活动期次及元素空间叠加模式上基本相同。两个钻孔中均出现了明显的“前尾晕共存”及“反向分带”现象。在此基础上结合微量元素垂向变化规律，分析了区内金矿体形成的热夜活动过程。研究表明两个钻孔的垂向分带都由两个完整的小循环组成，说明区内金矿体的形成至少经历了两次热夜活动叠加。
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