摘要
通过对新桥硫-多金属矿床含硫磁铁矿矿体赋存空间、构造环境、岩矿组合、围岩蚀变等宏观地质特征的研究,并结合微量元素,硫、铅、氢、氧同位素、矿物包体测温等资料综合分析认为:本区成矿物质来源为中深相幔源岩浆或同熔岩浆,进而研究矿床含硫磁铁矿体应属高温热液交代-后期热液叠加改造成因类型。
According to the features of the orebodies locations and associations of rocks and minerals ,and alterations of the wall rocks. The metallogenic geological conditions and process is investigated from field survey and analyses of trace elements and isotopes . It is proposed that the containing sulfur - magnetite orebody of this deposit belongs to the genetic type of the high temperature hydrothermal - alternate and hydrothermal superimposition.
出处
《化工矿产地质》
CAS
2003年第3期173-178,共6页
Geology of Chemical Minerals
关键词
地质特征
物源
成矿阶段
成矿机理
含硫磁铁矿
containing sulfur-magnetite orebody, Geological features, Genesis, Xin Qiao
