摘要
喇嘛苏铜矿床产于浅变质的库西姆契克群碳酸盐岩和海西期岩体的接触带附近，受地层、岩浆岩、构造等因素控制，有矽卡岩型、斑岩型、沉积型和热液充填型矿化；成矿物质既有来自地层的，也有来自深部岩浆的，成矿经历了多次富集和改造作用。因此，该矿床具有多成矿大地构造演化阶段、多控矿因素、多物质来源、多成因类型和多成矿作用的特点，是典型的多因复成矿床。
Occuring near the contact between the Kuximqiek carbonate rock and the Hercynian acidic bodies,the Lamasu copper deposit is controlled by strata,magmatic rock and structure.The metallizing features have skarn,porphyry,sedimentation and hydrothermal filled styles.The metallogenic material is from strata and deep－seated magma,it has undergone many metallizing stages.So,the ore deposit is characterized by many metallo－geotectonic evolution stages,mutiple ore－controlling factors,polymaterial sources,multiple metallogenesis and polygenetic types.It is a typical polygenetic compound deposit.
出处
《大地构造与成矿学》
EI
CAS
CSCD
北大核心
2001年第2期149-154,共6页
Geotectonica et Metallogenia
基金
国家305科技攻关项目 96─915─03─03
