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通过矿床地球化学特征和同位素年代学的研究，结合区域成矿规律分析，该矿床成矿物质主要来源于千里山花岗岩，成矿时代为燕山早期，成矿温度１６８℃～２４４℃，它属于岩浆期后中低温热液矿床。与柿竹园钨多金属矿、红旗岭锡（铅锌）矿、南风坳银（铅锌）矿共同组成一个完整的与千里山燕山早期花岗岩有关的矿床成矿系列。
Based on the study of geochemical characteristics and isotopic chronology and the analysis of regional metallogenic regularity, the ore-forming materials of this deposit mainly originate from the Thousandsilings granite. The mineralization age is early Yanshanian and the metallogenic temperature is 168 ℃ ~ 244 ℃. It belongs to the magma After the low temperature hydrothermal deposits. And the Shizhuyuan Tungsten polymetallic ore, Hongqi Ling tin (lead and zinc) mine, Nanfeng Au silver (lead-zinc) mine together to form a complete and thousands of miles of the Early Yanshanian granite-related mineralization series.