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Information Journal Paper

Title

Comparison of PGE concentration in the chromitites of Khoy Ophiolite: Its implication for the presence of two types of chromitites with two different origins

Pages

  273-286

Abstract

 Khoy ophiolitic complex in northwest of Iran have several chromitite bodies with various textures, different geochemical features and associated minerals. Based on Cr#, Khoy chromitites are divided into two groups: high-Cr (Cr# > 0. 6) and high-Al (Cr# < 0. 6) chromitites. The high-Cr contain some amount of PGEs with tiny grains of platinum-group minerals (PGM), whereas, high-Al chromitites are poor in PGE with no PGM inclusions. Geochemical analysis and Raman spectroscopy data on PGM inclusions in the high-Cr chromian spinels shows that they are laurite and rarely irarsite in composition. The PGE concentration in high-Cr-and high-Al chromitite reveals that the high-Cr chromitites probably were formed in a magmatic arc tectonic setting and those of high-Al were occurred in a back arc basin environment.

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    APA: Copy

    ZAEIMNIA, F., KANANIAN, A., MIRMOHAMMADI, M., & IMAMALIPOUR, A.. (2018). Comparison of PGE concentration in the chromitites of Khoy Ophiolite: Its implication for the presence of two types of chromitites with two different origins. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 26(2 ), 273-286. SID. https://sid.ir/paper/388178/en

    Vancouver: Copy

    ZAEIMNIA F., KANANIAN A., MIRMOHAMMADI M., IMAMALIPOUR A.. Comparison of PGE concentration in the chromitites of Khoy Ophiolite: Its implication for the presence of two types of chromitites with two different origins. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2018;26(2 ):273-286. Available from: https://sid.ir/paper/388178/en

    IEEE: Copy

    F. ZAEIMNIA, A. KANANIAN, M. MIRMOHAMMADI, and A. IMAMALIPOUR, “Comparison of PGE concentration in the chromitites of Khoy Ophiolite: Its implication for the presence of two types of chromitites with two different origins,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 26, no. 2 , pp. 273–286, 2018, [Online]. Available: https://sid.ir/paper/388178/en

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