Granite porphyry metallogenic system usually has been focued as a typical representative of "squeeze-type"- "Collision rift zone" marginal magma arc. Recent studies show that the porphyry tungsten molybdenum polymetallic metallogenic belt are controlled by a series of deep faults

produced in the vicinity of deep faults

Magmatic rift zone and On either side of the rift valley suture zone is an important metallogenic belt Vision which bred the Granite Porphyry Gold tungsten Molybdenum Polymetallic Deposits. Through the analysis of the metallogenic regularity of porphyry deposits

Further guidance granite porphyry gold prospecting direction of tungsten molybdenum polymetallic deposit.