Study of Phisico - Chemical Charactristic of Ore Bearing Fluidsin Fluorite of Kamar - Mehdi

Homoginization temperature of fluorite [luid indus ian indicate that mineralization has mostly take place within the temperature ranging 70 to 1500C . the last ice melting tcmpenttur ranges from 0 1O·2.2°C and shows that salinity varies from 0 to 3.69 wt% equivalent NaC!. Chemical analysis performed on The liquid phases of fluid indusion show that mineralizing fluids were rich in Ca and K. The above results along wilh data obtained by SEM equipped with EDAX spectrophotometery reveals that metal deposit of this mine were probably transported by chloride complexes. Temperature decrease and boiling accurancy were probably the cause of decomposition of chloride complex at the depusitiunal sites.