نویسنده
دانشکده فنی مهندسی بیرجند
چکیده
کلیدواژهها
عنوان مقاله [English]
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.
کلیدواژهها [English]
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