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Determination of Ore Forming Fluid’s Density of Fluorite Ore Deposits of Central Alborz

Author

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  • GHORBAN VAHABZADEH

    (Sari Agricultural Sciences and Natural Resources University, Sari, Iran)

  • SEYED HASSAN ZALI

    (Sari Agricultural Sciences and Natural Resources University, Sari, Iran)

Abstract

There are different ore deposits in Central Alborz which are distributed from east to west. Except Emaft fluorite ore deposit, other ore deposits in upper and middle members of Elika formation belong to Triassic age and are covered by Palan evaporated formation. The genesis of these deposits is considered as diagenetic to epigenetic. Fluorite reservoirs that are filled with faults or karst zones (open space filling) are originated in epigenetic. Layers and lenses are supposed as digenetic. From this fluorite a double polished thin section (polished wafers) was prepared and its salinity and homogenization temperature of fluid inclusion were tested using Linkham Tm 600 model. The results showed that in spite of the geographical distribution of ore deposits, their density is the same everywhere, but redeposit with digenetic or digenetic characteristic showed lower salinity. According to the salinity and homogenization temperature characteristics, these ore deposits are classified in Irish to MVT type.

Suggested Citation

  • Ghorban Vahabzadeh & Seyed Hassan Zali, 2016. "Determination of Ore Forming Fluid’s Density of Fluorite Ore Deposits of Central Alborz," International Journal of Applied and Physical Sciences, Dr K.Vivehananthan, vol. 2(2), pages 33-36.
    • Handle: RePEc:apa:ijapss:2016:p:33-36
    DOI: 10.20469/ijaps.2.50001-2.pdf
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