Based on summary of metallogenic geological background and deposit characteristics and fluid inclusion characteristics of ore of Qingshuihedonggou molybdenum deposit the paper discusses the metal-logenic model and genesis.The Mo deposit is a porphyry Mo deposit related to a shallow-uper-shallow porphyry intrusion.Monzogranite is the host rock.Layered,layeroid and lenticular Mo ore bodies occur in the porphyry and altered surrounding rock.Molybdenite occurs generally as scale aggregates or sporad-ic crystal in quartz veins or at the plane of fractures,rarely veinlets and dissemination in altered rock.Fluid inclusion of ore is characterized by high-low temperature,low salinity and low density.The Mo de-posit is formed under continent-continent collision and post collision extensional environment.Ore materi-als come from porphyry magma.This paper can provide reference for further study on regional metallo-genic law and prospecting.
porphyry Mo depositmetallogenic modelQingshuihedonggou Mo depositEast Kunlun areaQinghai province
维普
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