Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)

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, plag...

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Main Authors:	Saeed Kamran, Ahmad Jahangiri, Robab Hajialioghli, Mohsen Moayyed
Format:	Article
Language:	fas
Published:	University of Isfahan 2017-03-01
Series:	Petrology
Subjects:	Granite Peraluminous S-type syn-collision Ayghalesi Takab
Online Access:	http://ijp.ui.ac.ir/article_21499_5967c1a299002ff0cddb158d3a992249.pdf

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spelling	doaj-849c24a89b764e77990d77d44cbddeec2020-11-25T00:12:50ZfasUniversity of IsfahanPetrology2228-52102322-21822017-03-01829375210.22108/ijp.2017.2149921499Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)Saeed Kamran0Ahmad Jahangiri1Robab Hajialioghli2Mohsen Moayyed3Earth Sciences Department, Faculty of Natural Sciences, University of Tabriz, Tabriz, IranEarth Sciences Department, Faculty of Natural Sciences, University of Tabriz, Tabriz, IranEarth Sciences Department, Faculty of Natural Sciences, University of Tabriz, Tabriz, IranEarth Sciences Department, Faculty of Natural Sciences, University of Tabriz, Tabriz, IranThe 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 Key words: granite,http://ijp.ui.ac.ir/article_21499_5967c1a299002ff0cddb158d3a992249.pdfGranitePeraluminousS-typesyn-collisionAyghalesiTakab
collection	DOAJ
language	fas
format	Article
sources	DOAJ
author	Saeed Kamran Ahmad Jahangiri Robab Hajialioghli Mohsen Moayyed
spellingShingle	Saeed Kamran Ahmad Jahangiri Robab Hajialioghli Mohsen Moayyed Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran) Petrology Granite Peraluminous S-type syn-collision Ayghalesi Takab
author_facet	Saeed Kamran Ahmad Jahangiri Robab Hajialioghli Mohsen Moayyed
author_sort	Saeed Kamran
title	Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)
title_short	Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)
title_full	Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)
title_fullStr	Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)
title_full_unstemmed	Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)
title_sort	petrography and petrology of the ayghalesi granite, east of takab area (northwest of iran)
publisher	University of Isfahan
series	Petrology
issn	2228-5210 2322-2182
publishDate	2017-03-01
description	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 Key words: granite,
topic	Granite Peraluminous S-type syn-collision Ayghalesi Takab
url	http://ijp.ui.ac.ir/article_21499_5967c1a299002ff0cddb158d3a992249.pdf
work_keys_str_mv	AT saeedkamran petrographyandpetrologyoftheayghalesigraniteeastoftakabareanorthwestofiran AT ahmadjahangiri petrographyandpetrologyoftheayghalesigraniteeastoftakabareanorthwestofiran AT robabhajialioghli petrographyandpetrologyoftheayghalesigraniteeastoftakabareanorthwestofiran AT mohsenmoayyed petrographyandpetrologyoftheayghalesigraniteeastoftakabareanorthwestofiran
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Petrography and petrology of the Ayghalesi granite, east of Takab area (northwest of Iran)

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