摘要
Thoroughgoing studies of the homogenization temperatures, pressures and chendcal compositions offluid inclusions and the stable isotopes of hydrothermal minerals (quartz. calcite, pyrite and molybdenite)have thrown light on the evolution trend of the molybdenum-bearing hydrothermal system which originatedfrom magmatic processus and underwent significant mixing with meteoric waters in the later stages ofhydrothermal activity.
Thoroughgoing studies of the homogenization temperatures, pressures and chendcal compositions of fluid inclusions and the stable isotopes of hydrothermal minerals (quartz. calcite, pyrite and molybdenite) have thrown light on the evolution trend of the molybdenum-bearing hydrothermal system which originated from magmatic processus and underwent significant mixing with meteoric waters in the later stages of hydrothermal activity.
