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Geological Characteristics of East Gobi Molybdenum Deposit in Xinjiang and Hydrothermal Mineralization Stages and Mineral Paragenesis in the Deposit
详细信息   
摘要


     East Gobi molybdenum deposit in Xinjiang is the first super-large deposit discovered in north- west China. It is located near the Yamansu fault and occurrs in low grade metamorphic Lower Carbonifer- ous clastic rock intercalated with volcanic rocksl. According to cutting relation of ore veins hydrotrhermal mineralization in the deposit is divided into 4 stages and mineral paragenesus is determined on basis of cut- ting, replacement and edge share relation of the minerals.

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