摘要
云南澜沧铅锌银铜矿床为一多金属硫化物矿床。黄铁矿、闪锌矿及方铅矿为矿石中的主要金属矿物。黄铁矿中Co、Ni含量及Co/Ni比值较低,Se、Te和As含量较高。闪锌矿富Fe、Cd、In、贫Ga、Ge和Se。方铅矿含银较高,为银的主要载体矿物,贫Sb和Bi。矿物的微量元素标型特征反映出该矿床为一形成深度较浅的中温火山~次火山热液矿床。
Lancang Pb Zn Ag Cu deposit is a polymetallic sulfide deposit。Major metal min-erals in ore are pyrite,sphalerite and galena. Co and Ni contents and Co/Ni ratio are low and Se,Te ,As contents are high in pyrite.Sphalerite is enriched in Fe,Cd and In,but Ga,Ge adn Se contents are low,Galena is strongly enriched in silver and is main carryer of silver in ore,however Sb and Bi contents is very low,Mineral minor element model character-istics show that ore forming depth is shallow and the deposit is a volcanic subvolcanic mesothermal deposit.
出处
《西南工学院学报》
1995年第4期71-75,共5页
Journal of Southwest China Institute of Technology