摘要
下寒武统铅山组为矽卡岩型铅锌、铁多金属矿产的主要矿源层,被后期二长花岗岩侵入与变质岩系发生广泛接触交代作用,促使变质岩中的成矿物质活化。主要的容矿构造为断裂、矿体与地层接触面和不同期次界面。矿体与地层的接触界面是重要的控矿构造,主要为铅锌矿,有伴生金银、铜矿产出。
The Lower Cambrian Yanshan Formation is the main source bed of skarn Pb-Zn-Fe polymetallic minerals,which was extensively contacted and metasomatized by late monzonitic granite intrusion and metamorphic rock series, and promoted the activation of metallogenic materials in metamorphic rocks. The main ore hosting structures are faults, contact surfaces between ore bodies and strata and different stages of the interface. The interface between ore body and stratum is an important ore-controlling structure, mainly lead-zinc deposits, accompanied by gold, silver and copper deposits.
作者
索良明
李文龙
SUO Liang-ming;LI Wen-long(Team 707,Geological Exploration of Non-ferrous Metals in Heilongjiang Province,SuiHua 152000,China)
出处
《世界有色金属》
2018年第17期113-113,115,共2页
World Nonferrous Metals
关键词
车间南沟
铅锌矿
成矿远景
south ditch
lead-zinc deposit
metallogenic prospect