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Title

PETROGRAPHY AND PETROLOGY OF THE AYGHALESI GRANITE, EAST OF TAKAB AREA (NORTHWEST OF IRAN)

Pages

  37-52

Abstract

 The investigated GRANITE intrusion is located at the north of AYGHALESI village, east of TAKAB The AYGHALESI GRANITE has been intruded the Eocene sandstone and conglomerate rocks and low grade metamorphic hornfels have been metamorphosed host rocks. The main constituent minerals are K-feldspar, plagioclase, quartz and muscovite. and minor garnet. The main texture is granular but pegmatitic, myrmektitic, graphic and perthitic occur as minor textures. Chemically, the rocks are GRANITE on the various classification diagrams. The AYGHALESI intrusion body is classified as S-TYPE, PERALUMINOUS composition, calc-alkaline nature and is calcic-alkali to alkali-calcic on the base of modified alkali lime index (MALI). The investigated body, on the tectonic discrimination diagrams, fall on SYN-COLLISIONal tectonic setting domain, suggesting that it was originated during collision of Central Iranian and Arabian plates.

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    APA: Copy

    KAMRAN, SAEED, JAHANGIRI, AHMAD, HAJIALIOGHLI, ROBAB, & MOAYYED, MOHSEN. (2017). PETROGRAPHY AND PETROLOGY OF THE AYGHALESI GRANITE, EAST OF TAKAB AREA (NORTHWEST OF IRAN). PETROLOGY, 8(29 ), 37-52. SID. https://sid.ir/paper/196980/en

    Vancouver: Copy

    KAMRAN SAEED, JAHANGIRI AHMAD, HAJIALIOGHLI ROBAB, MOAYYED MOHSEN. PETROGRAPHY AND PETROLOGY OF THE AYGHALESI GRANITE, EAST OF TAKAB AREA (NORTHWEST OF IRAN). PETROLOGY[Internet]. 2017;8(29 ):37-52. Available from: https://sid.ir/paper/196980/en

    IEEE: Copy

    SAEED KAMRAN, AHMAD JAHANGIRI, ROBAB HAJIALIOGHLI, and MOHSEN MOAYYED, “PETROGRAPHY AND PETROLOGY OF THE AYGHALESI GRANITE, EAST OF TAKAB AREA (NORTHWEST OF IRAN),” PETROLOGY, vol. 8, no. 29 , pp. 37–52, 2017, [Online]. Available: https://sid.ir/paper/196980/en

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