Wulanwuzhuer-Shizisong ore deposit is a large Ag-polymetallic deposit newly discovered in the west part of the east KunlunShan ore belt in resent years.This paper deals with its metallogenic geological background,geological characteristics and metallogenic law and discusses the genesis.NW and nearly EW linear structure in the area is the ore-control structure.ore bodies are generally layeroid,veined,lenticu-lar.Ag,Pb and Zn ore is the main ore type.Galena,sphalerite,Fe-argentite and Fe-Cu argentite are the main ore minerals occurring as sparse dissemination and veins.Ore material is derived from rock-forming process of granitic porphyry.The deposit is formed under Late Triassic post collision extension environ-ment belonging to epigenetic-super epigenetic hydrothermal Ag polymetallic deposit.
Wulanwuzhuer Ag-polymetallic depositmetallogenic lawdeposit genesiseast Kunlun Shan area
万方数据
维普
