Abstract
Baoxingchang Cu-Mo deposit is one of several Cu-Mo-(Au) polymetallic deposits have been found in the Tethys metallogenic province. Laser-Raman spectral analysis shows that the vapour-phase components of fluid inclusions in quartz are mainly composed of water vapour and a little CO2, while the fluid-phase components contain Na+ and Cl− metallogenic fluid, which generally belongs to a NaCl-H2O system. In conclusion, the characteristics of fluid inclusions in porphyry-type Cu-Mo polymetallic deposits in Baoxingchang are closely related to multi-stage intrusions along the Jinshajiang-Red River shear zone.
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