内蒙古陈台屯斑岩型铜矿地质、地球物理特征及找矿方向  

Geological and Geophysical Characteristics of the Chentaitun Porphyry Copper Deposit in Inner Mongolia and Prospecting Direction

作　　者：刘鹤[1,2] 姚敬金 陈国华 李怀祥 高红刚 

机构地区：[1]中国地质大学(北京),北京100083 [2]中铁资源集团有限公司,北京100039

出　　处：《地质与勘探》2013年第4期654-664,共11页Geology and Exploration

基　　金：国家科技支撑计划课题(2011BAB04B09);教育部新世纪优秀人才支持计划(NCET-09-0710);北京市优秀博士学位论文指导老师科研项目(20111141501);高等学校学科创新引智计划(B07011);教育部长江学者和创新团队发展计划项目(IRT0755)联合资助;中铁资源地质勘查有限公司陈台屯铜多金属矿详查项目勘查经费的资助

摘　　要：内蒙古陈台屯铜矿区是一个以斑岩型铜矿为主要目标的勘查区,位于大兴安岭中段,成矿时代为中侏罗世。目前在矿区发现了斑岩型铜矿化和脉状铜矿化两种矿化类型。斑岩型铜矿化主要形成于陈台斑岩体顶部与二叠系大石寨组安山质火山岩的内、外接触带上,围岩蚀变作用强烈,并具有明显的分带特征,自下而上、由内到外可分为钾化带、黄铁-绢英岩化带、泥化带和青磐岩化带,斑岩型铜矿化主要集中于黄铁-绢英岩化带中。脉状铜矿主要充填于万宝组沉积地层和大石寨组火山岩的裂隙中,围岩蚀变仅发育黄铁-绢英岩化和弱青磐岩化。通过对矿区开展激电中梯测量和CSAMT电阻率测深并施工钻探验证,发现高极化率异常与斑岩型铜矿体和脉状铜矿体均具有良好的空间对应关系,可以作为下一步铜矿勘查的重要目标;低电阻率异常既可以由斑岩型铜矿化作用所引起,又可以由孔隙度较高的万宝组砂岩所引起,因此首先需要区分异常形成的原因,进而用低电阻率异常指导找矿,但高电阻率异常通常代表了致密的、不含矿的地质体。The Chentaitun copper district in Inner Mongolia, dominated by porphyry copper deposits, located in the middle section of the Hinggan Mountain, formed in middle Jurassic time. Two mineralization types have been identified ： porphyry copper mineralization and vein-style copper mineralizatinn. Porphyry copper mineralization occurred around the contact zones between the Pemaian Dashizhai Formation volcanoes and Chental porphyry intrusion, with intense wall-rock alteration. The alteration associated with porphyry copper mineralization can be divided into four zones from lower to upper or tYom inside to outside, which are potassie, quartz-serieite-pyrite （ QSP）, argillie and propylitic zones. Porphyry copper mineralization was predominantly concentrated in the QSP zone. Vein-type copper ores were filled within the fractures of the Wanbao Formation sedimentary strata and Dashizhai Formation volcanic rocks. Central gradient-aIway induced polarization and CSAMT survey results were verified by diamond drilling. It is concluded that high chargea- bility anomalies are spatially coincident with both pmT^hyry and vein-type copper orebodies. Therefore, the chargeability high could be key targets for the next stage of exploration. Low resistivity anomalies are not only caused by porphyry copper mineralization, but also generated by the Wanbao Formation sedimentary rocks of high porosity. It is necessary to investigate the reasons before applying the resistivity low to exploration targets. However, the high resistivity anomalies are usually associated with compact and barren geologic bodies.

关 键 词：斑岩型铜矿 围岩蚀变 地球物理特征 找矿方向 陈台屯 内蒙古 

分 类 号：P612[天文地球—矿床学]