摘要
通过对张家山铁矿床矿体与围岩的接触关系、蚀变特征、矿石的矿物组合、化学组分等地质特征及成因的分析研究,认为张家山铁矿床应属风化淋滤型铁矿床,其原生矿床为铁多金属硫化物矿床,并厘定了该地区铁矿的找矿标志。
Through the study of the relationship between the ore bodies and the country rocks, alteration, mineral association and chemical constituents in Zhangjiashan Iron Deposit, we think that Zhangjiashan Iron Deposit should be classified as weathering leaching type iron deposit, and the primary deposit should be a Fe polymetallic deposit. We have still collated and stipulated the indicators of iron deposit in this area.
出处
《华南地质与矿产》
CAS
2008年第2期43-48,共6页
Geology and Mineral Resources of South China
关键词
地质特征
矿床成因
找矿标志
张家山铁矿
Zhangjiashan iron deposit
Geological characteristics
genesis of deposit
indicators of prospecting
