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锡铁山铅锌矿床是50年代末期探明的大型块状硫化物矿床。80年代初开始矿山建设,并计划在“七五”期间进行采选。在此期间,西安地质矿产研究所在《锡铁山铅锌矿床类型与地质特征》课题研究中,发现有碳酸盐型锌矿石,继之青海地矿局中心实验室、长沙矿冶研究院、北京矿冶研究总院,西北矿冶研究院先后进行了实验研究工作,充分肯定该碳酸盐型锌矿石的矿物属Zn、Fe类质同象菱锌铁矿—菱铁锌矿系列矿物。在此基础上,笔者拟就该碳酸盐型锌矿石在矿床中的分布、产状、成分特征、成因以及工业利用问题谈些肤浅看法。
The Xieshan lead-zinc deposit is a large massive sulphide deposit proven in the late 1950s. In the early 1980s, the construction of mines began and plans are to be conducted during the “Seventh Five-Year Plan” period. During this period, Xi’an Institute of Geology and Mineral Resources in the “Xieshan lead-zinc deposits type and geological characteristics,” the subject of the study found that carbonate-type zinc ore, followed by Qinghai Bureau of Mines Central Laboratory, Changsha Institute of Mining and Metallurgy , Beijing Mining and Metallurgical Research Institute, Northwest Mining and Metallurgical Research Institute has carried out experimental research work, fully affirmed the carbonate zinc-bearing mineral zinc, Fe-like Ling-Ling ore with siderite - siderite series minerals . On this basis, I would like to make some brief comments on the distribution, occurrence, composition characteristics, causes and industrial utilization of the carbonate zinc ore in the deposit.