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Information Journal Paper

Title

MINERALOGY, PARAGENETIC RELATIONSHIPS AND INTRODUCING OF EQUILIBRIUM REACTIONS OF KUH-E-DOR SKARN, SOUTH-EAST OF YAZD

Pages

  87-105

Abstract

 The intrusion of Manshad diorite in Cretaceous carbonates of Shirkuh Mountain caused occurrences of KUH-E-DOR SKARN. Following mineral assemblage has been identified: Spinel+clintonite+phlogopite+pyroxene+garnet+vesuvianite.Paragenetic relationships show that there are a close association between spinel, CLINTONITE and phlogopite. Transition stage from magnesian to calcic SKARN is characterized by appearance of CLINTONITE. CLINTONITE restricted to low XCO2, SiO2 and high XH2O values of the coexisting fluids. Textural relationships of spinel with CLINTONITE-phlogopite show that spinel acted as precursor for genesis of these micas or they have been formed at the expense of spinel.spinel+SiO2+K2O+dolomite+H2O CLINTONITE+phlogopite Manshad SKARN is a polygenic SKARN in which pyroxene is formed at the first stage of mineralization followed by garnet and vesuvianite formation. Mineral assemblage of SKARN indicate temperature starting from maximum 800oC to 400oC which is followed by vesuvianite stability in XCO2<XH2O condition.

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    APA: Copy

    TAGHIPOUR, B.. (2012). MINERALOGY, PARAGENETIC RELATIONSHIPS AND INTRODUCING OF EQUILIBRIUM REACTIONS OF KUH-E-DOR SKARN, SOUTH-EAST OF YAZD. IRANIAN JOURNAL OF GEOLOGY, 5(20), 87-105. SID. https://sid.ir/paper/129368/en

    Vancouver: Copy

    TAGHIPOUR B.. MINERALOGY, PARAGENETIC RELATIONSHIPS AND INTRODUCING OF EQUILIBRIUM REACTIONS OF KUH-E-DOR SKARN, SOUTH-EAST OF YAZD. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2012;5(20):87-105. Available from: https://sid.ir/paper/129368/en

    IEEE: Copy

    B. TAGHIPOUR, “MINERALOGY, PARAGENETIC RELATIONSHIPS AND INTRODUCING OF EQUILIBRIUM REACTIONS OF KUH-E-DOR SKARN, SOUTH-EAST OF YAZD,” IRANIAN JOURNAL OF GEOLOGY, vol. 5, no. 20, pp. 87–105, 2012, [Online]. Available: https://sid.ir/paper/129368/en

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