摘要
沙丘地区铁多金属矿床位于祁漫塔格成矿带中,成矿地质条件优越。通过对沙丘地区铁多金属矿床成矿地质条件的分析及对矿床含矿特征的研究,探讨了矿床的成因。
Iron polymetallic deposit is located in the Shaqiu a^ea of Qimantage metallogenic belt, metallogenic geological condition is superior. Through the analysis of the geological conditions of iron polymetallie ore deposit in dune area and research on deposit ore characteristics, the paper discusses the genesis of the deposit.
出处
《价值工程》
2013年第9期285-287,共3页
Value Engineering
关键词
铁多金属矿
地质特征
矿床成因
沙丘地区
iron polymetallie ore deposit
geological characteristics
genesis
Shaqiu area
