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Title

MINERALOGICAL AND GEOCHEMICAL STUDIES AND DETERMINE THE PHYSICOCHEMICAL CONDITIONS OF THE KAN GOHAR REACTION SKARN, TUTAK, (BAVANAT-FARS)

Pages

  327-339

Abstract

 Kan Gohar REACTION SKARN is located at Sanandaj- Sirjan zone and is a part of TUTAK COMPLEX. Based on the field observations and petrographical studies, the deposit included granite-gneiss, micaschist, carbonate rock, and skarn, and Three zones, GARNETit skarn, amphibole and epidote skarn are classifications. Geochemically the intrusion is S-type, peraluminus and the nature of magma is calc-alkaline. Which located in the volcanic arc geological setting. Tutak intrusion is S-type; therefore it could not be related to the mineralization and skarnification. On the based of XRD results GARNET (ugrandites-pyralspites), calcite, hematite, magnetite, and dannemorite, magnesiohornblende are the main minerals. RARE EARTH ELEMENTS pattern in GARNETs shows two different patterns, can be indicator of presence of ugrandites and pyralspites GARNETs in the KAN GOHAR skarn. Ugrandites GARNETs (grossular-andradite), enrichment in LREE and depleted in HREE. Whereas, pyralspites GARNETs enrichment of HREE, and depletion of LREE. Based on geochemical studies the KAN GOHAR skarn were formed at T<500oC, fO2~ 10-21 and XCO2<0.2 bar.

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    APA: Copy

    TAGHIPOUR, BATOUL, TAGHVAEIFARD, MARYAM, & MACKIZADEH, MOHAMMAD ALI. (2015). MINERALOGICAL AND GEOCHEMICAL STUDIES AND DETERMINE THE PHYSICOCHEMICAL CONDITIONS OF THE KAN GOHAR REACTION SKARN, TUTAK, (BAVANAT-FARS). GEOCHEMISTRY, 3(4), 327-339. SID. https://sid.ir/paper/230890/en

    Vancouver: Copy

    TAGHIPOUR BATOUL, TAGHVAEIFARD MARYAM, MACKIZADEH MOHAMMAD ALI. MINERALOGICAL AND GEOCHEMICAL STUDIES AND DETERMINE THE PHYSICOCHEMICAL CONDITIONS OF THE KAN GOHAR REACTION SKARN, TUTAK, (BAVANAT-FARS). GEOCHEMISTRY[Internet]. 2015;3(4):327-339. Available from: https://sid.ir/paper/230890/en

    IEEE: Copy

    BATOUL TAGHIPOUR, MARYAM TAGHVAEIFARD, and MOHAMMAD ALI MACKIZADEH, “MINERALOGICAL AND GEOCHEMICAL STUDIES AND DETERMINE THE PHYSICOCHEMICAL CONDITIONS OF THE KAN GOHAR REACTION SKARN, TUTAK, (BAVANAT-FARS),” GEOCHEMISTRY, vol. 3, no. 4, pp. 327–339, 2015, [Online]. Available: https://sid.ir/paper/230890/en

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