摘要
研究区大地构造位于南邻东昆中新元古代—早古生代缝合带,成矿条件较好。白石崖M14铁多金属矿为接触交代型矽卡岩矿床。对矿区地层岩性、矿体形态、矿石类型、矿物组成、围岩蚀变等特征进行了详细总结,分析区内矿床的控矿因素和矿床成因,希望对今后的地质勘查工作有一定指导作用。
Geotectonics in the study area is located in the Mesoproterozoic-Early Paleozoic suture zone adjacent to East Kunming in the south,and the metallogenic conditions are good.Baishiya M14 iron polymetallic deposit is a contact metasomatic skarn deposit.The characteristics of strata,lithology,ore body shape,ore type,mineral composition and wall rock alteration in the mining area are summarized in detail.The ore-controlling factors and genesis of the deposits in the area are analyzed.It is hoped that this paper will play a guiding role in future geological exploration.
作者
冀春雨
于文明
孙靖宇
何广宇
JI Chun-yu;YU Wen-ming;SUN Jing-yu;HE Guang-yu(Comprehensive Census Brigade of North China Geological Survey Bureau,Langfang 065000,China)
出处
《世界有色金属》
2019年第17期86-88,共3页
World Nonferrous Metals
关键词
都兰
白石崖M14区
地质特征
矽卡岩型
矿床成因
dulan
baishiya M14 area
geological characteristics
skarn type
deposit genesis