Proceedings of GIA
TO GENESIS OF ZAGLIK ALUNITES FIELD OF DASHKESAN ORE REGION (ON ISOTOPIC RESEARCH DATA)
(I.A.Abdullayev, R.S.Jafarova, O.D.Bagirbekova)
According to research data of sulphur on isotopic level was defined that source of ore is tuffaceous series of alumosilicate rocks containing it.
Products of metasomatic processes in tuffaceous rocks leached and displaced from scarning zone and enriched by alumina and potassium formed Zaglik alunites field. The last ones are confined to Kimmeridge period with absolute age 141 MA and this was determined by K-Ar method.