• Geology
  • Published 2008

High salinity fluid characteristic and evolution of Xiaojiayingzi Mo (Fe) deposit,Liaoning province.

@inproceedings{Jun2008HighSF,
  title={High salinity fluid characteristic and evolution of Xiaojiayingzi Mo (Fe) deposit,Liaoning province.},
  author={Dai Jun and Mao Jing},
  year={2008}
}
Xiaojiayingzi Mo (Fe) deposit is temporally and spatially associated with intermediate to mafic rocks and the mineralization hosted in skarn.Fluid inclusion studies show that two types of primary fluid inclusion occur in calcite and quartz from molybdenite mineralization stage;daughter crystal-bearing polyphase inclusion and aqueous two-phase inclusion.The former homogenized to liquid phase by dissolution of daughter minerals,with homogenization temperatures from 203 to 440℃ and salinity… CONTINUE READING