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Information Journal Paper

Title

GEOCHEMICAL CHARACTERISTIC OF THE AMPHIBOLITE ROCKS OF PIR-EBAD, NE AZNA, SANANDAJ-SIRJAN ZONE

Pages

  16-32

Abstract

 Pir-abad amphibolotes in the northest Azna locates SANANDAJ- SIRJAN ZONE. The AMPHIBOLITEs show a discontinuous outcrops as pods and lenses. Sometimes have lineation and foliation. Amphibole and plagioclase are main mineral constituents in the rocks. The AMPHIBOLITEs have igneous source. Their protholite is basalt with sub-alkaline and tholeiitic nature. Chondrite normalized-REE diagram show LREE enrichment relatetoon to HREE. Primitive mantle- normalized trace elements diagram show depletion of HFSE and HREE. Tectonic discrimination diagrams, negative Nb-Ta anomalies and high Th and Ba/Yb display the back-arc basin setting or supra-subduction zone environment.

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  • Cite

    APA: Copy

    KOOLIVAND, SAHAR, SHABANIAN, NAHID, & DAVOUDIAN, ALI REZA. (2018). GEOCHEMICAL CHARACTERISTIC OF THE AMPHIBOLITE ROCKS OF PIR-EBAD, NE AZNA, SANANDAJ-SIRJAN ZONE. RESEARCHES IN EARTH SCIENCES, 8(32 ), 16-32. SID. https://sid.ir/paper/207446/en

    Vancouver: Copy

    KOOLIVAND SAHAR, SHABANIAN NAHID, DAVOUDIAN ALI REZA. GEOCHEMICAL CHARACTERISTIC OF THE AMPHIBOLITE ROCKS OF PIR-EBAD, NE AZNA, SANANDAJ-SIRJAN ZONE. RESEARCHES IN EARTH SCIENCES[Internet]. 2018;8(32 ):16-32. Available from: https://sid.ir/paper/207446/en

    IEEE: Copy

    SAHAR KOOLIVAND, NAHID SHABANIAN, and ALI REZA DAVOUDIAN, “GEOCHEMICAL CHARACTERISTIC OF THE AMPHIBOLITE ROCKS OF PIR-EBAD, NE AZNA, SANANDAJ-SIRJAN ZONE,” RESEARCHES IN EARTH SCIENCES, vol. 8, no. 32 , pp. 16–32, 2018, [Online]. Available: https://sid.ir/paper/207446/en

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