摘要
通过对银母寺铅锌矿矿体赋存状态，矿石结构、矿石中铅、硫同位素，微量元素分析及同类矿床对比，得出该矿床属“沉积－改造”层控矿床。
According to the inherent state of lead zinc deposit in Yinmusi,its ore structure, isotope of lead and zinc in ore, analysis of trace elements and comparison with the deposit of same kind, it follows that this belobgs to the sediment reforming strata bound deposit.
出处
《西安矿业学院学报》
北大核心
1996年第4期334-338,共5页
Journal of Xi'an University of Science & Technology
