It is considered a hypothermal Cu deposit based on ore body feature, mineralogy, texture and structure, wall rock alteration and genetic andlysis, then point out ore-searching directions.

• 根据矿体特征、矿石矿物成分、结构构造、围岩蚀变特征及成因分析，认为属中浅成高温热液型矿床，并指出找矿标志。