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Information Journal Paper

Title

MINERALOGY AND MINERAL CHEMISTRY OF SERPENTINITES AND METALISTVENITES IN THE BAYAZEH OPHIOLITE (NE OF ISFAHAN PROVINCE)

Pages

  729-742

Abstract

 The BAYAZEH OPHIOLITE, with probable Paleozoic age, is cropped out along the BAYAZEH fault and located in the eastern margin of the Yazd block (Central Iran). In the field, this OPHIOLITE consists of serpentinized peridotites, metagabbro, ultrabasic metamorphosed dikes, metapicrite, serpentinite and METALISTVENITE. Development of serpentinization process in the BAYAZEH mantle peridotites has been changed peridotites to serpentinized peridotite and serpentinite. Transitional transformation of serpentinite to METALISTVENITE is obvious in the field.Field and microscopic studies show that the METALISTVENITEs in the BAYAZEH OPHIOLITE have been produced by regional metamorphism from old listvenites. After old listvenite formation, during occurrence of regional metamorphism, carbonate listvenites changed to carbonate METALISTVENITEs and silica-carbonate listvenites changed to silica-carbonate METALISTVENITEs with abundant tremolite and actinolite. Chemistry of CR-SPINELs in the BAYAZEH serpentinites shows that they belong to depleted ophiolitic mantle peridotites.

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  • Cite

    APA: Copy

    NOSOUHIAN, N., & TORABI, GH.. (2014). MINERALOGY AND MINERAL CHEMISTRY OF SERPENTINITES AND METALISTVENITES IN THE BAYAZEH OPHIOLITE (NE OF ISFAHAN PROVINCE). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 21(4), 729-742. SID. https://sid.ir/paper/4106/en

    Vancouver: Copy

    NOSOUHIAN N., TORABI GH.. MINERALOGY AND MINERAL CHEMISTRY OF SERPENTINITES AND METALISTVENITES IN THE BAYAZEH OPHIOLITE (NE OF ISFAHAN PROVINCE). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2014;21(4):729-742. Available from: https://sid.ir/paper/4106/en

    IEEE: Copy

    N. NOSOUHIAN, and GH. TORABI, “MINERALOGY AND MINERAL CHEMISTRY OF SERPENTINITES AND METALISTVENITES IN THE BAYAZEH OPHIOLITE (NE OF ISFAHAN PROVINCE),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 21, no. 4, pp. 729–742, 2014, [Online]. Available: https://sid.ir/paper/4106/en

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