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مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Information Journal Paper

Title

GEOCHEMISTRY AND PETROGENESIS OF THE ORZUIEH VOLCANIC SEQUENCE (SOUTH OF IRAN)

Pages

  65-76

Abstract

 The Late Jurassic to Early Cretaceous ORZUIEH volcanic sequence is exposed in the southern part of the SANANDAJ - SIRJAN ZONE. Major and trace element geochemistry shows magma evolution from the transitional to the calc-alkaline series. Clinopyroxene compositions are similar to their composition in subduction setting and support a VOLCANIC ARC related environment. REE and trace element diagrams show enrichment patterns in LREE relative to HREE and depletion in Nb and Ta elements. This magmatic sequence has been originated from the mantle source with effect of liquids and sediment resulted from the subducting slab. The ORZUIEH volcanic sequence is probably originated during the subduction of the Neo-Tethyan Oceanic lithosphere under the SANANDAJ - SIRJAN ZONE, during the Late Jurassic to Early Cretaceous time, in the VOLCANIC ARC tectonic environment.

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    APA: Copy

    MONSEF, I., RAHGOSHAY, M., & EMAMI, M.H.. (2012). GEOCHEMISTRY AND PETROGENESIS OF THE ORZUIEH VOLCANIC SEQUENCE (SOUTH OF IRAN). GEOSCIENCES, 21(82), 65-76. SID. https://sid.ir/paper/32515/en

    Vancouver: Copy

    MONSEF I., RAHGOSHAY M., EMAMI M.H.. GEOCHEMISTRY AND PETROGENESIS OF THE ORZUIEH VOLCANIC SEQUENCE (SOUTH OF IRAN). GEOSCIENCES[Internet]. 2012;21(82):65-76. Available from: https://sid.ir/paper/32515/en

    IEEE: Copy

    I. MONSEF, M. RAHGOSHAY, and M.H. EMAMI, “GEOCHEMISTRY AND PETROGENESIS OF THE ORZUIEH VOLCANIC SEQUENCE (SOUTH OF IRAN),” GEOSCIENCES, vol. 21, no. 82, pp. 65–76, 2012, [Online]. Available: https://sid.ir/paper/32515/en

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