Wedge-Shaped Pop-Up Structure in the Eslami Peninsula, Lake Urmia, Northwestern Iran
Ancient subduction zones are characterized by metamorphic and orogenic belts. The Zagros Orogenic Belt comprises almost all sections of an ancient subduction zone along which Neo-Tethyan oceanic crust was subducted beneath central Iran. The Eslami Peninsula, as a part of the Zagros Orogenic Belt in...
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| Veröffentlicht in: | Acta geologica Sinica (Beijing) Jg. 91; H. 4; S. 1264 - 1269 |
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| Format: | Journal Article |
| Sprache: | Englisch |
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Wiley Subscription Services, Inc
01.08.2017
Department of Geology, Faculty of Science, Urmia University, Urmia 57153-165, Iran |
| Ausgabe: | English ed. |
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| ISSN: | 1000-9515, 1755-6724 |
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| Abstract | Ancient subduction zones are characterized by metamorphic and orogenic belts. The Zagros Orogenic Belt comprises almost all sections of an ancient subduction zone along which Neo-Tethyan oceanic crust was subducted beneath central Iran. The Eslami Peninsula, as a part of the Zagros Orogenic Belt in Azerbaijan province, northwestern Iran, is situated between the Lake Urmia fore-arc basin and the Sahand Magmatic Arc. This region contains Eocene leucite dikes, trachyte, tephrite, phenolite, basanite and syenite. Volcanic features related to the Sahand are located in the eastern part of the Eslami Peninsula. In view of its relative age and composition, the Eslami Peninsula proposed as an outer arc of the Sahand Magmatic Arc that formed within the post-collisional setting of the central Iranian and Arabian plates. After subduction and contact of the two plates, a symmetric pop-up structure has been created by thrusting in the Zagros belt as a result of the collision processes. The injesction of dikes in the Eslami Peninsula is also a result of the continent continent collision. |
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| AbstractList | Ancient subduction zones are characterized by metamorphic and orogenic belts. The Zagros Orogenic Belt comprises almost all sections of an ancient subduction zone along which Neo‐Tethyan oceanic crust was subducted beneath central Iran. The Eslami Peninsula, as a part of the Zagros Orogenic Belt in Azerbaijan province, northwestern Iran, is situated between the Lake Urmia fore‐arc basin and the Sahand Magmatic Arc. This region contains Eocene leucite dikes, trachyte, tephrite, phenolite, basanite and syenite. Volcanic features related to the Sahand are located in the eastern part of the Eslami Peninsula. In view of its relative age and composition, the Eslami Peninsula proposed as an outer arc of the Sahand Magmatic Arc that formed within the post‐collisional setting of the central Iranian and Arabian plates. After subduction and contact of the two plates, a symmetric pop‐up structure has been created by thrusting in the Zagros belt as a result of the collision processes. The injesction of dikes in the Eslami Peninsula is also a result of the continent_continent collision. |
| Author | Akram ALIZADEH Fayezeh JANGJOO |
| AuthorAffiliation | Department of Geology, Faculty of Science, Urmia University, Urmia 57153-165, Iran |
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| Cites_doi | 10.1016/j.gr.2013.09.015 10.1016/j.jseaes.2005.01.003 10.1016/j.crte.2010.07.005 10.1144/GSL.SP.2003.210.01.01 10.1016/j.chemer.2006.04.002 10.1016/j.tecto.2012.01.022 10.1144/GSL.SP.1989.044.01.02 10.1029/2002JB002190 10.1016/j.jseaes.2010.02.008 |
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| DocumentTitleAlternate | Wedge-Shaped Pop-Up Structure in the Eslami Peninsula, Lake Urmia, Northwestern Iran |
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| Keywords | Eslami Peninsula Lake Urmia Sahand Zagros post-collision |
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| Notes | Eslami Peninsula, Lake Urmia, Sahand, post-collision, Zagros 11-2001/P Ancient subduction zones are characterized by metamorphic and orogenic belts. The Zagros Orogenic Belt comprises almost all sections of an ancient subduction zone along which Neo-Tethyan oceanic crust was subducted beneath central Iran. The Eslami Peninsula, as a part of the Zagros Orogenic Belt in Azerbaijan province, northwestern Iran, is situated between the Lake Urmia fore-arc basin and the Sahand Magmatic Arc. This region contains Eocene leucite dikes, trachyte, tephrite, phenolite, basanite and syenite. Volcanic features related to the Sahand are located in the eastern part of the Eslami Peninsula. In view of its relative age and composition, the Eslami Peninsula proposed as an outer arc of the Sahand Magmatic Arc that formed within the post-collisional setting of the central Iranian and Arabian plates. After subduction and contact of the two plates, a symmetric pop-up structure has been created by thrusting in the Zagros belt as a result of the collision processes. The injesction of dikes in the Eslami Peninsula is also a result of the continent continent collision. Ar About the first author Dr. Akram Alizadeh is Assistant Professor in the Department of Geology, Urmia University, Iran. She specializes in structural geology, tectonics and active tectonism. Her doctoral thesis at Shiraz University was on a “gneiss dome” within the Zagros Orogenic Belts under the supervision of Dr. Khalil Sarkarinejad. She did Ar geochronological dating with Dr. Margarita Lopez‐Martinez at CICESE, Mexico, during the sabbatical leave associated with her doctoral studies. She is the author or coauthor of 13 papers on the geology of western Iran. 40 39 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 |
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| References | 2012; 532–535 2003; 108 2010; 39 2006; 26 2009 2010; 342 2014; 26 1995 2008; 68 2006 2003 2002 1989 Gadirzadeh A. (e_1_2_2_4_1) 2002 e_1_2_2_14_1 e_1_2_2_5_1 e_1_2_2_11_1 e_1_2_2_10_1 Soltani Gh. (e_1_2_2_12_1) 2006 Storti F. (e_1_2_2_13_1) 2003 e_1_2_2_2_1 e_1_2_2_3_1 Kearey P. (e_1_2_2_6_1) 2009 e_1_2_2_9_1 e_1_2_2_8_1 Khodabandeh A.A. (e_1_2_2_7_1) 1995 |
| References_xml | – start-page: 3 year: 1989 end-page: 15 – year: 2009 – volume: 108 start-page: 2840 issue: B10 year: 2003 article-title: Deformation of brittle‐ductile thrust wedges in experiments and nature publication-title: Journal of Geophysical Research – volume: 342 start-page: 837 year: 2010 end-page: 846 article-title: Ar‐ Ar Geochronology in a gneiss dome within the Zagros orogenic Belt publication-title: Comptes Rendus Geosciences – year: 2002 – year: 2006 – year: 2003 – volume: 26 start-page: 683 year: 2006 end-page: 693 article-title: A new tectonic scenario for the Sanandaj‐Sirjan Zone (Iran) publication-title: Journal of Asian Earth Sciences – year: 1995 – volume: 39 start-page: 37 year: 2010 end-page: 50 article-title: Petrogenesis of Plio‐Quaternary post‐collisional ultrapotassic volcanism in NW of Maraud, NW Iran publication-title: Journal of Asian Earth Sciences – volume: 68 start-page: 141 year: 2008 end-page: 154 article-title: Geochemistry and petrogenesis of lamprophyric dykes and the associated rocks from Eslami peninsula, NW Iran: Implications for deep mantle metasomatism publication-title: Chemie der Erde – volume: 26 start-page: 1028 issue: 3–4 year: 2014 end-page: 1050 article-title: Late Miocene K‐rich volcanism in the Eslamieh Peninsula (Saray), NW Iran: implications for geodynamic evolution of the Turkish‐Iranian High Plateau publication-title: Gondwana Research – volume: 532–535 start-page: 27 year: 2012 end-page: 60 article-title: Building the Zagros collisional orogen: Timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence publication-title: Tectonophysics – ident: e_1_2_2_10_1 doi: 10.1016/j.gr.2013.09.015 – ident: e_1_2_2_5_1 doi: 10.1016/j.jseaes.2005.01.003 – volume-title: Osku, Geological Quadrangle Map, 1:100,000 scale year: 1995 ident: e_1_2_2_7_1 – ident: e_1_2_2_3_1 doi: 10.1016/j.crte.2010.07.005 – volume-title: Orumiyeh, Geological Quadrangle Map, 1:100,000 scale year: 2006 ident: e_1_2_2_12_1 – volume-title: Intraplate strike‐slip deformation belts year: 2003 ident: e_1_2_2_13_1 doi: 10.1144/GSL.SP.2003.210.01.01 – ident: e_1_2_2_8_1 doi: 10.1016/j.chemer.2006.04.002 – ident: e_1_2_2_9_1 doi: 10.1016/j.tecto.2012.01.022 – ident: e_1_2_2_14_1 doi: 10.1144/GSL.SP.1989.044.01.02 – ident: e_1_2_2_11_1 doi: 10.1029/2002JB002190 – ident: e_1_2_2_2_1 doi: 10.1016/j.jseaes.2010.02.008 – volume-title: Global Tectonics year: 2009 ident: e_1_2_2_6_1 – volume-title: Azarshahr, Geological Quadrangle Map, 1:100,000 scale year: 2002 ident: e_1_2_2_4_1 |
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| Snippet | Ancient subduction zones are characterized by metamorphic and orogenic belts. The Zagros Orogenic Belt comprises almost all sections of an ancient subduction... Ancient subduction zones are characterized by metamorphic and orogenic belts.The Zagros Orogenic Belt comprises almost all sections of an ancient subduction... |
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| SubjectTerms | Composition Dikes Embankments Eocene Eslami Peninsula Lake Urmia Lakes Magma Oceanic crust Orogeny Plate tectonics Plates (tectonics) post‐collision Potassium aluminum silicates Sahand Subduction Subduction (geology) Subduction zones Syenite Trachyte Zagros 伊朗 古俯冲带 楔形 洋壳俯冲 结构 西北部 造山带 阿拉伯板块 |
| Title | Wedge-Shaped Pop-Up Structure in the Eslami Peninsula, Lake Urmia, Northwestern Iran |
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