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Information Journal Paper

Title

MINERAL CHEMISTRY AND THERMOBAROMETRY OF MANTLE PERIDOTITE IN THE OPHIOLITIC MELANGE OF NORTHWEST OF BIRJAND, EAST OF IRAN

Pages

  355-368

Abstract

 The study area is located in northwest of BIRJAND, northern part of the SISTAN SUTURE ZONE in eastern Iran. There is well preserved outcrops of an ophiolite melange in this area. This complex is composed of HARZBURGITE, layered gabbro and spilitic basalt with flysch type rocks.Microprobe analyses of olivine, clinopyroxene, orthopyroxene and spinel in HARZBURGITEs show that olivine is forsterite (Fo90.15-Fo90.75), clinopyroxene is diopsidic augite (Mg#=95.8), orthopyroxene is enstatite (Mg#=91.58), and spinel (Cr#=41) is Al-Cr bearing type. Based on THERMOBAROMETRY of clinopyroxene and orthopyroxene minerals, crystallization temperature of peridotites is 1016±100 oC at 25 Kbar pressure.

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    APA: Copy

    SALIMI, Z., ZARRINKOUB, M.H., & MOHAMMADI, S.S.. (2013). MINERAL CHEMISTRY AND THERMOBAROMETRY OF MANTLE PERIDOTITE IN THE OPHIOLITIC MELANGE OF NORTHWEST OF BIRJAND, EAST OF IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 21(2), 355-368. SID. https://sid.ir/paper/3847/en

    Vancouver: Copy

    SALIMI Z., ZARRINKOUB M.H., MOHAMMADI S.S.. MINERAL CHEMISTRY AND THERMOBAROMETRY OF MANTLE PERIDOTITE IN THE OPHIOLITIC MELANGE OF NORTHWEST OF BIRJAND, EAST OF IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2013;21(2):355-368. Available from: https://sid.ir/paper/3847/en

    IEEE: Copy

    Z. SALIMI, M.H. ZARRINKOUB, and S.S. MOHAMMADI, “MINERAL CHEMISTRY AND THERMOBAROMETRY OF MANTLE PERIDOTITE IN THE OPHIOLITIC MELANGE OF NORTHWEST OF BIRJAND, EAST OF IRAN,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 21, no. 2, pp. 355–368, 2013, [Online]. Available: https://sid.ir/paper/3847/en

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