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  • Role of supra-subduction zone ophiolites in the tectonic evolution of the southeastern Zagros Orogenic Belt, Iran

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عنوان URL للمقالة


رقم المقالة : IJES-1611-1067 (R1) زيارة : 105 الصفحة: 31 - 38

نوع المخطوط: ابحاث

Role of supra-subduction zone ophiolites in the tectonic evolution of the southeastern Zagros Orogenic Belt, Iran

الموضوعات :

Ramin Arfania 1 (Department of Geology, Faculty of Basic Sciences, Islamic Azad University, Isfahan (Khorasgan Branch))

تاريخ الإرسال : 28 الإثنين , صفر, 1438 تاريخ التأكيد : 14 الأربعاء , محرم, 1439 تاريخ الإصدار : 15 الأحد , رجب, 1439

الکلمات المفتاحية: Sanandaj-Sirjan, Ophiolite, Supra-subduction zone, Zagros Orogenic Belt,

ملخص المقالة :

Ophiolitic rocks in the southeastern part of the Zagros Orogenic Belt can be separated from southwest to northeast, into two groups: the Neyriz ophiolites and the Naien–Shahrebabak–Baft ophiolites. The southeast sector of Sanandaj-Sirjan wasdelimited by the two nearly synchronous ophiolitic belts in its southwestern and northeastern margins. In this study, new ophiolitic formation models were used to explain a viable geodynamic hypothesis on the development of the southeastern Zagros Orogenic Belt. Supra-subduction zone ophiolites have been of particular importance in the reconstruction of regional tectonic evolution andformed near a main subducting oceanic plate. The history of the southeastern Zagros Orogenic Belt is composed of development of two oceanic crusts, referred to as the Neo-Tethys 1 and Neo-Tethys 2. The process of reconstructingof the plate tectonic evolution of the southeastern Zagros Orogenic Belt was proposed on the basis of "Latest Cretaceous-Neogene collision" hypothesis. The supra-subduction zone ophiolites in the southeastern part of the Zagros Orogenic Belt can be classified into "pull related fore-arc Neyriz ophiolites" and "back-arc Naien-Baft ophiolites".

المصادر:


  1. Ahmad T, Posht-Kuhi M (1993) Geochemisty and petrogenesis of Urumiah–Dokhtar volcanics around Naien and Rafsanjan areas: a preliminary study, Treatise on the Geology of Iran. Tehran, Iranian Ministry of Mines and Metals, 90 p.
    2.
  2. Alavi M (1994) Tectonic of Zagros orogenic belt of Iran: new data and interpretations, Tectonophysics 229: 211-238.
    3.
  3. Alavi M (2004) Regional stratigraphy of the Zagros folded-thrust belt of Iran and its proforeland evolution, American Journal of Science 304: 1-20.
    4.
  4. Amidi SM, Emami MH, Michel R (1984) Alkaline character of Eocene volcanism in the middle part of Central Iran and its geodynamic situation, Geologische Rundschau 73: 917-926.
    5.
  5. Arfania R, Shahriari S (2009) Role of southeastern Sanandaj–Sirjan Zone in the tectonic evolution of Zagros Orogenic Belt, Iran, Island Arc 18: 555-576.
    6.
  6. Azizi H, Chung SL, Tanaka T, Asahara Y (2011) Isotopic dating of the Khoy metamorphic complex (KMC), northwestern Iran: A significant revision of the formation age and magma source, Precambrian Research 185: 87-94.
    7.
  7. Babaie HA, Ghazi AM, Babaie A, La Tour TE, Hassanipak AA (2001) Geochemistry of arc volcanic rocks of the Zagros Crush Zone, Neyriz, Iran, Journal of Asian Earth Sciences 19: 61-76.
    8.
  8. Babaie HA, Ghazi A, Babaei A, Duncan R, Mahony J, Hassanipak A (2003) New Ar-Ar age, isotopic and geochemical data for basalts in the Neyriz ophiolite, Iran, Geophysical Research Abstracts 5: 12899.
    9.
  9. Babaie HA, Ghazi AM, Babaei A, Arvin M (2006) Geochemical, 40Ar/39Ar age, and isotopic data for crustal rocks of the Neyriz ophiolite, Iran, Canadian Journal of Earth Sciences 43: 57-70.
    10.
  10. Babaei A, Arvin M, Babaie HA (2001) An oblique convergence and rotation model for the emplacement of the Baft ophiolitic mélange in Iran, Ofioliti 26: 404-408.
    11.
  11. Berberian M (1976) Seismotectonic 1:2500000 Map of Iran, Tehran, Geological Survey of Iran.
    12.
  12. Berberian F, Muir ID, Pankhurst RJ, Berberian M (1982) Late Cretaceous and Early Miocene Andean-Type Plutonic Activity in Northern Makran and Central Iran, Journal of Geological Society London 139: 605-614.
    13.
  13. Berberian M (1983) The Southern Caspian: A Compressional Depression Floored by a Trapped, Modified Oceanic Crust, Canadian Journal of Earth Sciences 20, 163-183.
    14.
  14. Berberian M, King GCP (1981) Towards a paleogeography and tectonic evolution of Iran, Canadian  Journal of Earth Sciences 18: 210-265.
    15.
  15. Coleman RG (1981). Tectonic setting for ophiolite obduction in Oman, Journal of Geophysics Research 86: 2497-2508.
    16.
  16. Colman-Sadd SP (1978) Fold development in Zagros simply folded belt, southwest Iran, American Association of Petroleum Geologists Bulletin 62: 984-1003.
    17.
  17. Desmons J, Beccaluva L (1983) Mid-ocean ridge and island-arc affinities in ophiolites from Iran, palaeographic implications, Chemical Geology 39: 39-63.
    18.
  18. Dilek Y, Furnes H (2009) Structure and geochemistry of Tethyan ophiolites and their petrogenesis in subduction rollback systems, Lithos 113: 1–20.
    19.
  19. Dimitrijevic M (1973) Geology of Kerman region. Institute for Geological and Mining Exploration and Institution of Nuclear and Other Mineral Raw Materials. Belgrad Yugoslavia, 334 p.
    20.
  20. Eftekharnejad J (1981) Tectonic division of Iran with respect to sedimentary basins, Journal of Iranian Petroleum Society 82: 19-28.
    21.
  21. Falcon NL (1974) Southern Iran–Zagros Mountains, In: Anthony Mansell Spencer, (Ed.), Mesozoic–Cenozoic orogenic belts. Geological Society, London, Special Publications 4: 199-211.
    22.
  22. Fakhari MD, Axen GJ, Horton BK, Hassanzadeh J, Amini A (2008) Revised age of proximal deposits in the Zagros foreland basin and implications for Cenozoic evolution of the High Zagros, Tectonophysics 451: 170-185.
    23.
  23. Farhoudi G A (1978) Comparison of Zagros Geology to Island Arcs, Journal of Geology 86: 323-334.
    24.
  24. Forster H, Fesefeldt K, Kursten M, Germany FR (1972) Magmatic and orogenic evolution of the Central Iranian volcanic belt, 24th. IGC. Section 2, 198-209.
    25.
  25. Gansser A (1974) The ophiolitic mélange, a world-wide problem on Tethyan examples, Ecologae Geologica Helvetica 67: 479-507.
    26.
  26. Ghasemi A, Talbot CJ (2006) A new tectonic scenario for the Sanandaj-Sirjan Zone (Iran), Journal of Asian Earth Sciences 26: 683-693.
    27.
  27. Ghazi AM, Hassanipak AA (1999) Geochemistry, petrology and the origin of Shahr-Babak Ophiolite, Central Iran, Ofioliti 24: 96-107.
    28.
  28. Glennie K W (2000) Cretaceous tectonic evolution of Arabia’s eastern plate margin: A tale of two oceans, In: Abdulrahman S. Alsharhan, Scott, R.W. (Eds.), Middle East models of Jurassic/Cretaceous carbonate systems. Society of Economic Paleontologists and Mineralogists, Special Publication 69: 9-20.
    29.
  29. Golonka J (2007) Geodynamic evolution of the South Caspian Basin, In: P. O. Yilmaz, Isaksen, G. H. (Eds.), Oil and gas of the Greater Caspian area, American Association of Petroleum Geologists, Studies in Geology 55: 17–41.
    30.
  30. Hassanipak AA, Ghazi AM (2000). Petrochemistry, 40Ar–39Ar ages and tectonics of the Nain Ophiolite, Central Iran. In: GSA Annual Meeting, 237–238 pp.
    31.
  31. Hassanipak AA, Ghazi M, Duncan R, Pessagno EA, Kariminia SM, Mobasher K (2003) Spatial and temporal distribution of Paleo- and Neo-Tethys ophiolites in Iran and their tectonomagmatic significance, Geological Society of America Abs. with Prog 34: 331.
    32.
  32. Hessami K, Koyi HA, Talbot CJ, Tabasi H, Shabanian E (2001) Progressive unconformities within an evolving foreland fold- thrust belt, Zagros Mountains, Journal of Geological Society London 158: 969-981.
    33.
  33. Jackson J, McKenzie D (1984) Active tectonics of the Alpine-Himalayan belt between western Turkey and Pakistan, Geophysical Journal of the Royal Astronomical Society 77: 185-264.
    34.
  34. Jung D, Kūrsten M, Tarkian M (1976) Post-Mesozoic volcanism in Iran and its relation to the subduction of the Afro-Arabian under the Eurasian plate. In: Andreas P, Rosler A. (Eds.), Afar Between Continental and Oceanic Rifting, Stuttgart, Schweizerbartsche Verlagbuchhandlung, 216.
    35.
  35. Lippard SJ, Shelton AW, Gass IG (1986) The ophiolite of northern Oman, Geological Society London Memoir 76:141-176.
    36.
  36. Mouthereau F, Tensi J, Bellahsen N, Lacombe O, De Boisgrollier T, Kargar S (2007) Tertiary sequence of deformation in a thin-skinned/thick-skinned collision belt: The Zagros Folded Belt (Fars, Iran), Tectonics 26: 1-27.
    37.
  37. Nouri F, Azizi H, Golonka J, Asahara Y, Orihashi Y, Yamamoto K, Tsuboi M, Anma R (2016) Age and petrogenesis of Na-rich felsic rocks in western Iran: evidence for closure of the southern branch of the Neo-Tethys in the Late Cretaceous, Tectonophysics 671: 151-172.
    38.
  38. Ricou LE (1971) Le croissant ophiolitique péri-arabe. Une ceinture de nappes mises en place au Crétacé supérieur, Rev. Geogr. Phys. Géol. Dyn. 13: 327-350.
    39.
  39. Ruban DA, Al-Husseini MI, Iwasaki Y (2007) Review of Middle East paleozoic plate tectonics, GeoArabia 12: 35-56.
    40.
  40. Şengör AMC (1990) A new model for the late Palaeozoic-Mesozoic tectonic evolution of Iran and implications for Oman, In: Robertson AHF., Searle MP, Ries AC. (Eds.), the geology and tectonics of the Oman region, Geological Society, London, Special Publications 49: 797-831.
    41.
  41. Shafaii-Moghadam H, Stern RJ (2015) Ophiolites of Iran: Keys to understanding the tectonic evolution of SW Asia: (II) Mesozoic ophiolites, Journal of Asian Earth Sciences 100, 31-59
    42.
  42. Shafaii-Moghadam H, Whitechurch H, Rahgoshay M, Monsef I (2009) Significance of Nain– Baft ophiolitic belt (Iran): short-lived, transitional Cretaceous back-arc oceanic basins over the Tethyan subduction zone, C. R. Geoscience 341: 1016-1028.
    43.
  43. Shahabpour J (2005) Tectonic evolution of the orogenic belt in the region located between Kerman and Neyriz, Journal of Asian Earth Sciences 24: 405-417.
    44.
  44. Shahabpour J (2007) Island-arc affinity of the Central Iranian Volcanic Belt, Journal of Asian Earth Sciences 30: 652-665.
    45.
  45. Sheikholeslami MR, Pique A, Mobayen P, Sabzehie M, Bellon H, Emami MH (2008) Tectono-metamorphic evolution of the Neyriz metamorphic complex, Quri-Kor-e-Sefid area, (Sanandaj- Sirjan Zone, SW Iran), Journal of Asian Earth Sciences 31: 504-521.
    46.
  46. Stern RJ (2004) Subduction initiation: Spontaneous and induced, Earth and Planetary Science Letters 226: 275-292.
    47.
  47. Stِcklin J (1968) Structural history and tectonics of Iran: A review, American Association of Petroleum Geologists Bulletin 52: 1229-1258.
    48.
  48. Stِcklin J (1974) Possible ancient continental margin in Iran, In: Creighton Burk, Drake, C.L. (Eds.), The Geology of Continental Margins. Berlin, Springer, 873-887.
    49.
  49. Stِcklin J (1977) Structural correlation of the Alpine ranges between Iran and central Asia. Memoire Hors-Serie de la Societe Geologique de France 8: 333-353.
    50.
  50. Stoneley R (1990) The Arabian continental margin in Iran during the Late Cretaceous, In: Alastair Robertson, Searle, M., Ries, A. (Eds.), The Geology and Tectonics of the Oman Region. Geological Society, London, Special Publications 49: 787-795.
    51.
  51. Taraz H (1974) Geology of the Surmagh-Deh Bid area, Abadeh region, central Iran. Tehran, Geological Survey of Iran Report 37: 104.  
    52.
  52. Topuz G, Gِçmengil G, Rolland Y, اelik F, Zack T, Schmitt AK (2013) Jurassic accretionary complex and ophiolite from northeast Turkey: No evidence for the Cimmerian continental ribbon, Geology 41: 255-258.
    53.

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