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Information Journal Paper

Title

GEOCHEMICAL AND TECTONOMAGMATIC ANALYSIS OF DIBASIC DIKES AND BASALTIC LAVAS IN THE NOORABAD OPHIOLITE (NORTH-WEST LORESTAN)

Pages

  83-101

Abstract

 The NOORABAD OPHIOLITE is a part of Eastern Mediterranean-Zagros-Oman Tethyan OPHIOLITEs, cropping out in south-southwest of the Main Zagros Thrust fault. In this sequence of the OPHIOLITE rocks, DIABASE DIKES and BASALTIC LAVAS are widespread. The chemical composition of these rocks comprise sub-alkaline basalts, andesitic basalt and andesite. According to normalized REE diagrams to the chondrite and trace elements normalized to the primitive mantle, these rocks show calc-alkaline series, the enrichment of LREE and LILE and depletion of HFSE elements. The characteristics of these OPHIOLITEs are similar to other exposed Tethyan OPHIOLITEs along Bitlis-Zagros suture zone, and their formation is associated with SUPRA-SUBDUCTION ZONEs.

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    Cite

    APA: Copy

    AHMADI KHALAJI, A., KINANI, M., KAMALI, Z., SHAFAHII MOGHADAM, H., & TAHMASBI, Z.. (2016). GEOCHEMICAL AND TECTONOMAGMATIC ANALYSIS OF DIBASIC DIKES AND BASALTIC LAVAS IN THE NOORABAD OPHIOLITE (NORTH-WEST LORESTAN). IRANIAN JOURNAL OF GEOLOGY, 10(38), 83-101. SID. https://sid.ir/paper/129305/en

    Vancouver: Copy

    AHMADI KHALAJI A., KINANI M., KAMALI Z., SHAFAHII MOGHADAM H., TAHMASBI Z.. GEOCHEMICAL AND TECTONOMAGMATIC ANALYSIS OF DIBASIC DIKES AND BASALTIC LAVAS IN THE NOORABAD OPHIOLITE (NORTH-WEST LORESTAN). IRANIAN JOURNAL OF GEOLOGY[Internet]. 2016;10(38):83-101. Available from: https://sid.ir/paper/129305/en

    IEEE: Copy

    A. AHMADI KHALAJI, M. KINANI, Z. KAMALI, H. SHAFAHII MOGHADAM, and Z. TAHMASBI, “GEOCHEMICAL AND TECTONOMAGMATIC ANALYSIS OF DIBASIC DIKES AND BASALTIC LAVAS IN THE NOORABAD OPHIOLITE (NORTH-WEST LORESTAN),” IRANIAN JOURNAL OF GEOLOGY, vol. 10, no. 38, pp. 83–101, 2016, [Online]. Available: https://sid.ir/paper/129305/en

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