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Information Journal Paper

Title

GARNET GENESIS IN ALTERED CONGLOMERATE OF SANGESTAN FORMATION, DAMAK ALIABAD (WEST OF TAFT, YAZD PROVINCE)

Pages

  263-278

Abstract

 The conglomerates of SANGESTAN FORMATION (Lower Cretaceous) have been metamorphosed in the vicinity of the leucogranitoid rocks of the Shir-Kuh batholith and have created the mineral assemblage of GARNET- epidote-quartz-calcite-pyrite in the contact halo. Following the contact metamorphism, hydrothermal alteration (pyrite formation and silicification) has likely occurred. Based on the trace element contents of the GARNETs, the SKARN in the contact halo is Cu-Pb-Zn bearing calcic SKARN type. The above mentioned minerals, apparently, indicate that there is a genetic relationship between intrusions related Cu-mineralization and the SKARNification in the study area.

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    Cite

    APA: Copy

    ASAD ELAHI, P., KHALILI, M., & MAKIZADEH, M.A.. (2007). GARNET GENESIS IN ALTERED CONGLOMERATE OF SANGESTAN FORMATION, DAMAK ALIABAD (WEST OF TAFT, YAZD PROVINCE). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 14(2), 263-278. SID. https://sid.ir/paper/3936/en

    Vancouver: Copy

    ASAD ELAHI P., KHALILI M., MAKIZADEH M.A.. GARNET GENESIS IN ALTERED CONGLOMERATE OF SANGESTAN FORMATION, DAMAK ALIABAD (WEST OF TAFT, YAZD PROVINCE). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2007;14(2):263-278. Available from: https://sid.ir/paper/3936/en

    IEEE: Copy

    P. ASAD ELAHI, M. KHALILI, and M.A. MAKIZADEH, “GARNET GENESIS IN ALTERED CONGLOMERATE OF SANGESTAN FORMATION, DAMAK ALIABAD (WEST OF TAFT, YAZD PROVINCE),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 14, no. 2, pp. 263–278, 2007, [Online]. Available: https://sid.ir/paper/3936/en

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