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The Sanandaj-Sirjan zone of Iran is a metamorphic belt consisting of rocks which were metamorphosed under different pressure and temperature conditions and intruded by various plutons ranging in composition from gabbro to granite. The majority of these granitoids formed along the an-cient active continental margin of the Neo-Tethyan ocean at the southeastern edge of the central Ira-nian microplate. Geochronological data published in recent years indicate periodic plutonism lasting from Carboniferous through Mesozoic to late-Paleogene times (from ca. 300 to ca. 35 Ma) with cli-max activity during the mid- and late-Jurassic. The age constraints for plutonic complexes, such as Siah-Kouh, Kolah-Ghazi, Golpayegan (Muteh), Azna, Aligoodarz, Astaneh, Borujerd, Malayer (Samen), Alvand, Almogholagh, Ghorveh, Saqqez, Marivan, Naqadeh and Urumieh, clearly indicate the periodic nature of magmatism. Therefore, the Sanandaj-Sirjan zone preserves the record of mag-matic activity of a complete orogenic cycle related to (1) Permocarboniferous(?) rifting of Gondwana and opening of the Neo-Tethyan ocean, (2) subduction of the oceanic crust, (3) continental collision and (4) post-collision/post-orogenic activities. The formation of the Marivan granitoids, northwestern Sanandaj-Sirjan zone, for which we present U-Pb zircon and titanite ages of ca. 38 Ma, can be related to the collisional and post-collisional stages of this orogenic cycle.
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Tom
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207--215
Opis fizyczny
Bibliogr. 39 poz., rys., tab.
Twórcy
autor
- Department of Geology, Bu-Ali Sina University, Hamedan, Iran
autor
- Department of Geology, Bu-Ali Sina University, Hamedan, Iran
autor
- Department of Earth Sciences, University of Tübingen, Tübingen, Germany
autor
- Department of Geology, Bu-Ali Sina University, Hamedan, Iran
Bibliografia
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- 16.Esna-Ashari A, Tiepolo M, Valizadeh MV, Hassanzadeh J and Sepahi AA, 2012. Geochemistry and zircon U–Pb geochronology of Ali-goodarz granitoid complex, Sanandaj-Sirjan zone, Iran. Journal of Asian Earth Sciences 43(1): 11–22, DOI 10.1016/j.jseaes.2011.09.001.
- 17.Frost BR, Barnes CG, Collins WJ, Arculus RJ, Ellis DJ and Frost CD, 2001. A Geochemical classification for granitic rocks. Journal of Petrology 42(11): 2033–2048, DOI 10.1093/petrology/42.11.2033.
- 18.Ghalamghash J, Nédélec A, Bellon H, Vousoughi-Abedini M and Bouchez JL, 2009. The Urumieh plutonic complex (NW Iran): A record of the geodynamic evolution of the Sanandaj–Sirjan zone during Cretaceous times-Part I: Petrogenesis and K/Ar dating. Journal of Asian Earth Sciences 35(5): 401–415, DOI 10.1016/j.jseaes.2009.02.002.
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- 22.Mansouri-Esfahani M, Khalili M, Kochhar N and Gupta LN, 2010. A-type granite of the Hasan-Robat area (NW of Isfahan, Iran) and its tectonic significance. Journal of Asian Earth Sciences 37(3): 207–218, DOI 10.1016/j.jseaes.2009.05.010.
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- 24.Mazhari SA, Amini S, Ghalamghash J and Bea F, 2012. Petrogenesis of granitic unit of Naqadeh complex, Sanandaj-Sirjan Zone, NW Iran. Arabian Journal of Geosciences 4(1–2): 59–67, DOI 10.1007/s12517-009-0077-6.
- 25.Mazhari SA, Bea F, Amini S, Ghalamghash J., Molina JF, Montero P, Scarrow JH and Williams IS, 2009. The Eocene Bimodal Pi-ranshahr Massif of the Sanandaj-Sirjan Zone, NW Iran: A Marker of the End of the Collision in the Zagros Orogen. Journal of the Geological Society 166(1): 53–69, DOI 10.1144/0016-76492008-022.
- 26.Moazzen M, Moayyed M, Modjarrad M and Darvishi E, 2004. Azna granitoid as an example of syn-collision S-type granitisation in Sanandaj-Sirjan metamorphic belt, Iran. Neues Jahrbuch fuer Mi-neralogie Monatschafte 11: 489–507.
- 27.Mohajjel M and Fergusson CL, 2000. Dextral transpression in late Cretaceous continental collision, Sanandaj-Sirjan zone, western Iran. Journal of Structural Geology 22(8): 1125–1139, DOI 10.1016/S0191-8141(00)00023-7.
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- 31.Ranin A, 2009. Petrogensis of plutonic bodies and metamorphic rocks in the Marivan area. M. Sc. Thesis (in Persian), Bu-Ali Sina University, Iran.
- 32.Ranin A, Sepahi AA, Moein-Vaziri H and Aliani F, 2010. Petrology and geochemistry of the plutonic complexes of the Marivan area, Sanandaj-Sirjan zone (In Farsi with English abstract). Journal of Petrology, Isfahan University, Iran 2: 43–60.
- 33.Saccani E, Allahyari K, Beccaluva L and Bianchini G, 2013. Geochem-istry and petrology of the Kermanshah ophiolites (Iran): Implica-tion for the interaction between passive rifting, oceanic accretion, and OIB-type components in the Southern Neo-Tethys Ocean. Gondwana Research 24(1): 392–411, DOI 10.1016/j.gr.2012.10.009.
- 34.Sepahi AA, 2008. Typology and petrogenesis of granitic rocks in the Sanandaj-Sirjan metamorphic belt, Iran: with emphasis on the Al-vand plutonic complex. Neues Jahrbuch Geologie Und Paleontologie, Abhandlungen 247(3): 295–312.
- 35.Shahbazi H, Siebel W, Pourmoafee M, Ghorbani M, Sepahi AA, Shang CK and Vousoughi-Abedini M, 2010. Geochemistry and U–Pb zircon geochronology of the Alvand plutonic complex in Sanan-daj–Sirjan Zone (Iran): New evidence for Jurassic magmatism. Journal of Asian Earth Sciences 39(6): 668–683, DOI 10.1016/j.jseaes.2010.04.014.
- 36.Stacey JS and Kramers JD, 1975. Approximation of terrestrial lead isotope evolution by a two stage model. Earth and Planetary Sci-ence Letters 26(2): 207–221, DOI 10.1016/0012-821X(75)90088-6.
- 37.Sun JF, Yang JH, Wu FY, Xie LW, Yang YH, Liu ZC and Li XH, 2012. In situ U-Pb dating of titanite by LA-ICPMS, Chinese Science Bul-letin 57(20): 2506–2516, DOI 10.1007/s11434-012-5177-0.
- 38.Valizadeh MV and Cantagrel JM, 1975. Premieres donnees radi-ometriques (K-Ar et Rb-Sr) sur les micas du complexe magma-tique du Mont Alvand pres Hamedan (Iran Occidental). Comptes Rendus Hebdomadares des Seances de l’Academie des Sciences, Serie D. Sciences Naturelles 281: 1083–1086.
- 39.Zhang LS and Schärer U, 1996. Inherited Pb components in magmatic titanite and their consequence for the interpretation of U–Pb ages. Earth and Planetary Science Letters 138(1–4): 57–65, DOI 10.1016/0012-821X(95)00237-7.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-82a4d232-1db3-4bd8-996f-1e764216be57