摘要
内蒙古自治区锡林郭勒盟西乌旗道伦达坝中型铜多金属矿床位于大兴安岭南段西坡,矿体主要产于粉砂质板岩与黑云母花岗岩的接触带。本文通过系统的岩相学、矿相学、流体包裹体和氢、氧同位素研究表明,道伦达坝铜多金属矿床属岩浆期后气化热液矿床,成矿过程包括早、中、晚3个阶段,温度区间分别为388～>500℃、302～463℃、179～359℃。钨-锡矿化主要发生在中阶段、铜矿化主要发生在晚阶段。初始成矿流体为CH_4-CO_2-H_2O-NaCl体系,随着温压降低,CO_2、CH_4大量逸失,而演化为H_2O-NaCl体系。流体盐度变化范围大,但从早到晚逐步降低。流体临界分离导致钨、锡矿化;流体CH_4、CO_2逃逸和大气降水热液混入导致铜矿化。黑云母花岗岩的侵入活动导致了成矿流体的聚集,而粉砂质板岩有利于成矿流体封闭,致使二者接触带成为有利的成矿和找矿部位。
The Daolundaba medium-sized Copper-poly-metal deposit in Xiwuzhumuqin Qi,Xilinguole City,Inner Mongolia,occurs in the western Great Xing an Range.Ore-bodies are mainly hosted in the contact zone between a biotite granite and a silty slate.The study in ore petrography and fluid inclusions and hydrogen oxygen isotope geochemistry shows that the Daolundaba deposit was formed by post-magmatic hydrothermal process.Hydrothermal mineralization are divided into the early,middle and late stages with homogenization t...
出处
《岩石学报》
SCIE
EI
CAS
CSCD
北大核心
2009年第11期2957-2972,共16页
Acta Petrologica Sinica
基金
国家973项目(2006CB403501)
中国地质调查局项目(1212010813045)资助
关键词
流体包裹体
氢氧同位素
成矿流体
道伦达坝铜多金属矿
内蒙古
Fluid inclusions
Hydrogen and oxygen isotopes
Ore-forming fluids
Daolundaba copper-poly-metal deposit
Inner Mongolia
