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Information Journal Paper

Title

MINERALOGY, THERMOBAROMETRY AND TECTONIC SETTING INTERPRETATION OF GNEISSES FROM WESTERN SOLTAN ABAD (NE SABZEVAR)

Pages

  227-240

Abstract

 The study area is situated in the west of SOLTAN ABAD prom NE SABZEVAR (Razavi Khorasan province). There is an exposure of metamorphic complex that contains green schist, blue schist, and amphibolite and eclogite (?) facieses rocks. GNEISSic body is located in the middle part of this complex (Koh-e-Chili). Protolithic and foliation intensity are variable in this body.Field evidences, whole rock geochemistry, geochronological data and nearly the same metamorphic pressure conditions of GNEISSes and blue schist’s (Gneiss: P=10.9 Kb and Blue schist: P=11-14 Kb) indicate that protolith of the GNEISSes have been differentiated series of oceanic crust and have experienced seduction zone metamorphism along with mafic series of SABZEVAR oceanic basin (blue schists) as a consequence of north-ward movement of central Iranian micro continent in the Upper Eocene.

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  • Cite

    APA: Copy

    RAZAVI, S.M.H., & NASRABADY, M.. (2011). MINERALOGY, THERMOBAROMETRY AND TECTONIC SETTING INTERPRETATION OF GNEISSES FROM WESTERN SOLTAN ABAD (NE SABZEVAR). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 19(2), 227-240. SID. https://sid.ir/paper/4082/en

    Vancouver: Copy

    RAZAVI S.M.H., NASRABADY M.. MINERALOGY, THERMOBAROMETRY AND TECTONIC SETTING INTERPRETATION OF GNEISSES FROM WESTERN SOLTAN ABAD (NE SABZEVAR). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2011;19(2):227-240. Available from: https://sid.ir/paper/4082/en

    IEEE: Copy

    S.M.H. RAZAVI, and M. NASRABADY, “MINERALOGY, THERMOBAROMETRY AND TECTONIC SETTING INTERPRETATION OF GNEISSES FROM WESTERN SOLTAN ABAD (NE SABZEVAR),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 19, no. 2, pp. 227–240, 2011, [Online]. Available: https://sid.ir/paper/4082/en

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