Geochemistry and petrogenesis of Eocene shoshonitic ‎and adakitic volcanic rocks in Sonajeel area ‎(Southeast of Heris, Eastern Azerbaijan)‎

The studied area is located in the SE of Heris (Eastern Azerbaijan province) and the Alborz-Azerbaijan structural zone. The Eocene volcanic rocks in the area of under study show various compositions ranging from olivine basalt, hornblende basalt, basaltic andesite and andesite to trachy andesite. Th...

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Main Authors: Nasibeh Nemati, Mehraj Aghazadeh, Zahra Badrzadeh
Format: Article
Language:fas
Published: University of Isfahan 2018-11-01
Series:Petrology
Subjects:
Online Access:http://ijp.ui.ac.ir/article_23077_89186ddc4ac4d9043ac1fb82ee5e8ef7.pdf
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spelling doaj-a5759af1604345a3b212be255bb6ce0a2020-11-25T01:47:13ZfasUniversity of IsfahanPetrology2228-52102322-21822018-11-019314717210.22108/ijp.2018.104987.103723077Geochemistry and petrogenesis of Eocene shoshonitic ‎and adakitic volcanic rocks in Sonajeel area ‎(Southeast of Heris, Eastern Azerbaijan)‎Nasibeh Nemati0Mehraj Aghazadeh1Zahra Badrzadeh2Department of Geology, Payameh Noor UniversityDepartment of Geology, Payameh Noor University, East Azarbaijan‎Department of Geology, Payameh Noor University, East Azarbaijan‎The studied area is located in the SE of Heris (Eastern Azerbaijan province) and the Alborz-Azerbaijan structural zone. The Eocene volcanic rocks in the area of under study show various compositions ranging from olivine basalt, hornblende basalt, basaltic andesite and andesite to trachy andesite. The studied basaltic rocks, except for amphibole types, which show calc-alkaline affinity, mainly have shoshonitic and the andesitic rocks are adakitic composition. According to primitive mantle and chondrite normalized spider and REE diagrams, the studied rocks are characterized by LILE and LREE enrichment and pronounced depletion in HFS elements. Based on geochemical data the basaltic rocks have been originated from different degrees partial melting of a heterogeneous lithospheric mantle that metasomatized by subduction agents. The adakitic rocks have been generated from partial melting of thickened potassic mafic lower crust that have been metamorphosed in eclogitic facies.http://ijp.ui.ac.ir/article_23077_89186ddc4ac4d9043ac1fb82ee5e8ef7.pdfshoshoniteadakitepetrogenesiseocenesonajeelarasbaran
collection DOAJ
language fas
format Article
sources DOAJ
author Nasibeh Nemati
Mehraj Aghazadeh
Zahra Badrzadeh
spellingShingle Nasibeh Nemati
Mehraj Aghazadeh
Zahra Badrzadeh
Geochemistry and petrogenesis of Eocene shoshonitic ‎and adakitic volcanic rocks in Sonajeel area ‎(Southeast of Heris, Eastern Azerbaijan)‎
Petrology
shoshonite
adakite
petrogenesis
eocene
sonajeel
arasbaran
author_facet Nasibeh Nemati
Mehraj Aghazadeh
Zahra Badrzadeh
author_sort Nasibeh Nemati
title Geochemistry and petrogenesis of Eocene shoshonitic ‎and adakitic volcanic rocks in Sonajeel area ‎(Southeast of Heris, Eastern Azerbaijan)‎
title_short Geochemistry and petrogenesis of Eocene shoshonitic ‎and adakitic volcanic rocks in Sonajeel area ‎(Southeast of Heris, Eastern Azerbaijan)‎
title_full Geochemistry and petrogenesis of Eocene shoshonitic ‎and adakitic volcanic rocks in Sonajeel area ‎(Southeast of Heris, Eastern Azerbaijan)‎
title_fullStr Geochemistry and petrogenesis of Eocene shoshonitic ‎and adakitic volcanic rocks in Sonajeel area ‎(Southeast of Heris, Eastern Azerbaijan)‎
title_full_unstemmed Geochemistry and petrogenesis of Eocene shoshonitic ‎and adakitic volcanic rocks in Sonajeel area ‎(Southeast of Heris, Eastern Azerbaijan)‎
title_sort geochemistry and petrogenesis of eocene shoshonitic ‎and adakitic volcanic rocks in sonajeel area ‎(southeast of heris, eastern azerbaijan)‎
publisher University of Isfahan
series Petrology
issn 2228-5210
2322-2182
publishDate 2018-11-01
description The studied area is located in the SE of Heris (Eastern Azerbaijan province) and the Alborz-Azerbaijan structural zone. The Eocene volcanic rocks in the area of under study show various compositions ranging from olivine basalt, hornblende basalt, basaltic andesite and andesite to trachy andesite. The studied basaltic rocks, except for amphibole types, which show calc-alkaline affinity, mainly have shoshonitic and the andesitic rocks are adakitic composition. According to primitive mantle and chondrite normalized spider and REE diagrams, the studied rocks are characterized by LILE and LREE enrichment and pronounced depletion in HFS elements. Based on geochemical data the basaltic rocks have been originated from different degrees partial melting of a heterogeneous lithospheric mantle that metasomatized by subduction agents. The adakitic rocks have been generated from partial melting of thickened potassic mafic lower crust that have been metamorphosed in eclogitic facies.
topic shoshonite
adakite
petrogenesis
eocene
sonajeel
arasbaran
url http://ijp.ui.ac.ir/article_23077_89186ddc4ac4d9043ac1fb82ee5e8ef7.pdf
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