摘要
通过对青海德尔尼硫化物矿床的产出部位、成矿环境、矿石矿物的组合、主要化学元素的成份及同位素测试数据等分析研究,认为该矿床具有裂谷成矿机制的特征,成因类型应属裂谷型层控矿床。
Through the studies of produced position, metallogenic surrounding, mineralassemblages of ore, main chemical composition, and isotopic date, et al., the author holdthat Deerni sulfide deposit is characterized by rift-type metallogenic mechanism, its genetictype should be belong to a rift-type stratabound ore deposit.
