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Information Journal Paper

Title

THE COMPOSIONAL ZONING OF GARNET IN ECLOGITES FROM NORTH OF SHAHREKORD, SANANDAJ - SIRJAN ZONE, IRAN

Pages

  271-286

Abstract

 The metabasite rocks from north of Shahrekord, which is a part of structural zone of Sanandaj-Sirjan, are undergone medium temperature - high pressure metamorphism (ECLOGITE facies). These rocks then were subjected to a retrograde metamorphism (amphibolite facies). A distinct COMPOSITIONAL ZONING is preserved in fresh GARNETs which are formed during ECLOGITE facies. The compositional or growth zoning in these ECLOGITE rocks shows clockwise P-T-t path. In the beginning of metamorphism, P and T increased up to reach to the peak of high pressure metamorphism, then P decreased while the T was increasing during uplift and decompression. These growth stages indicate that Pmax was not contemporaneous with Tmax during ECLOGITE facies metamorphism of the metabasites from North of Shahrekord, in Sanandaj - Sirjan Zone.

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    APA: Copy

    DAVOUDIAN DEHKORDI, A.R., KHALILI, M., NOURBEHESHT, I., & MOHAJEL, MOHAMMAD. (2006). THE COMPOSIONAL ZONING OF GARNET IN ECLOGITES FROM NORTH OF SHAHREKORD, SANANDAJ - SIRJAN ZONE, IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 13(2), 271-286. SID. https://sid.ir/paper/4221/en

    Vancouver: Copy

    DAVOUDIAN DEHKORDI A.R., KHALILI M., NOURBEHESHT I., MOHAJEL MOHAMMAD. THE COMPOSIONAL ZONING OF GARNET IN ECLOGITES FROM NORTH OF SHAHREKORD, SANANDAJ - SIRJAN ZONE, IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2006;13(2):271-286. Available from: https://sid.ir/paper/4221/en

    IEEE: Copy

    A.R. DAVOUDIAN DEHKORDI, M. KHALILI, I. NOURBEHESHT, and MOHAMMAD MOHAJEL, “THE COMPOSIONAL ZONING OF GARNET IN ECLOGITES FROM NORTH OF SHAHREKORD, SANANDAJ - SIRJAN ZONE, IRAN,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 13, no. 2, pp. 271–286, 2006, [Online]. Available: https://sid.ir/paper/4221/en

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