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Title

MINERAL CHEMISTRY OF THE CORDIERITE, SPINEL AND ANDALUSITE OF KOLAH GHAZI GRANITOID BODY (S-SE ISFAHAN)

Pages

  251-257

Abstract

 Kolah Ghazi granitoid body located in Sanandaj-Sirjan zone is composed of quartz, plagioclase, K-felds-par, biotite and accessory minerals such as tourmaline, cordierite, andalusite, sillimanite, kyanite, spinel and garnet. Based on microprobe analyses, cordierites of the study area are of high temperature and low pressure metamorphic type formed in expense of biotite during antexis of pelitic rocks. The spinels are hercynite in composition and derived from metamorphic of enriched-Fe sediments. The formation of symplectic intergrowth texture of spinel in the rims of andalusite and cordierite may be related to the reaction between andalusite and the adjacent biotites. This may be an indication of imbalance condition caused by pressure reduction from tectonic movements. The inherited A/CNK from host pelitic rocks is responsible for crystallization of andalusite.

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    APA: Copy

    SAFARI MIRGHALEH, AFSANEH, KHALILI, MAHMOUD, MANSOURI ESFAHANI, MAHIN, & KHALILI, KHADIJEH. (2013). MINERAL CHEMISTRY OF THE CORDIERITE, SPINEL AND ANDALUSITE OF KOLAH GHAZI GRANITOID BODY (S-SE ISFAHAN). GEOCHEMISTRY, 1(3), 251-257. SID. https://sid.ir/paper/230861/en

    Vancouver: Copy

    SAFARI MIRGHALEH AFSANEH, KHALILI MAHMOUD, MANSOURI ESFAHANI MAHIN, KHALILI KHADIJEH. MINERAL CHEMISTRY OF THE CORDIERITE, SPINEL AND ANDALUSITE OF KOLAH GHAZI GRANITOID BODY (S-SE ISFAHAN). GEOCHEMISTRY[Internet]. 2013;1(3):251-257. Available from: https://sid.ir/paper/230861/en

    IEEE: Copy

    AFSANEH SAFARI MIRGHALEH, MAHMOUD KHALILI, MAHIN MANSOURI ESFAHANI, and KHADIJEH KHALILI, “MINERAL CHEMISTRY OF THE CORDIERITE, SPINEL AND ANDALUSITE OF KOLAH GHAZI GRANITOID BODY (S-SE ISFAHAN),” GEOCHEMISTRY, vol. 1, no. 3, pp. 251–257, 2013, [Online]. Available: https://sid.ir/paper/230861/en

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