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Jinfeng Sun, Jin-Hui Yang, Fu-guan Wu, Liewen Xie, Yue-heng Yang, Zhi‐Chao Liu, Xian‐Hua Li (2012)
In situ U-Pb dating of titanite by LA-ICPMSChinese Science Bulletin, 57
A. Sepahi (2008)
Typology and petrogenesis of granitic rocks in the Sanandaj-Sirjan metamorphic belt, Iran: with emphasis on the Alvand plutonic complexNeues Jahrbuch Fur Geologie Und Palaontologie-abhandlungen, 247
(1975)
Premieres donnees radi - ometriques ( KAr et Rb - Sr ) sur les micas du complexe magma - tique du Mont Alvand pres Hamedan ( Iran Occidental )
A. Khalaji, D. Esmaeily, M. Valizadeh, H. Rahimpour-Bonab (2007)
Petrology and geochemistry of the granitoid complex of Boroujerd, Sanandaj-Sirjan Zone, Western IranJournal of Asian Earth Sciences, 29
M. Mohajjel, C. Fergusson (2000)
Dextral transpression in Late Cretaceous continental collision, Sanandaj–Sirjan Zone, western IranJournal of Structural Geology, 22
A Ranin, AA Sepahi, H Moein-Vaziri, F Aliani (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
P. Agard, J. Omrani, L. Jolivet, H. Whitechurch, B. Vrielynck, W. Spakman, P. Monié, B. Meyer, R. Wortel (2011)
Zagros orogeny: a subduction-dominated processGeological Magazine, 148
S. Mazhari, F. Bea, Sadraldin Amini, J. Ghalamghash, José Molina, Pilar Montero, J. Scarrow, I. Williams (2009)
The Eocene bimodal Piranshahr massif of the Sanandaj–Sirjan Zone, NW Iran: a marker of the end of the collision in the Zagros orogenJournal of the Geological Society, 166
H. Azizi, Tsuyoshi Tanaka, Y. Asahara, Sun‐Lin Chung, M. Zarrinkoub (2011)
Discrimination of the age and tectonic setting for magmatic rocks along the Zagros thrust zone, northwest Iran, using the zircon U–Pb age and Sr–Nd isotopesJournal of Geodynamics, 52
R. Parrish (1987)
An improved micro-capsule for zircon dissolution in UPb geochronologyChemical Geology: Isotope Geoscience Section, 66
J. Braud (1987)
La Suture du Zagros au niveau de Kermanshah (Kurdistan iranien) : reconstitution paléogéographique : évolution géodynamique, magmatique et structurale
J. Ghalamghash, A. Nédélec, H. Bellon, M. Abedini, J. Bouchez (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 datingJournal of Asian Earth Sciences, 35
E. Saccani, K. Allahyari, L. Beccaluva, G. Bianchini (2013)
Geochemistry and petrology of the Kermanshah ophiolites (Iran): Implication for the interaction between passive rifting, oceanic accretion, and OIB-type components in the Southern Neo-Tethys OceanGondwana Research, 24
M Alavi (1994)
Tectonics of Zagros orogenic belt of Iran: New data and interpretationTectonophysics, 229
F. Bea, Ali Mazhari, P. Montero, Sadraldin Amini, J. Ghalamghash (2011)
Zircon dating, Sr and Nd isotopes, and element geochemistry of the Khalifan pluton, NW Iran: Evidence for Variscan magmatism in a supposedly Cimmerian superterraneJournal of Asian Earth Sciences, 40
S. Mazhari, Sadraldin Amini, J. Ghalamghash, F. Bea (2011)
Petrogenesis of granitic unit of Naqadeh complex, Sanandaj–Sirjan Zone, NW IranArabian Journal of Geosciences, 4
Vahid Ahadnejad, M. Valizadeh, R. Deevsalar, M. Rezaei‐Kahkhaei (2011)
Age and geotectonic position of the Malayer granitoids: Implication for plutonism in the Sanandaj-Sirjan Zone, W IranNeues Jahrbuch Fur Geologie Und Palaontologie-abhandlungen, 261
J. Stacey, J. Kramers (1975)
Approximation of terrestrial lead isotope evolution by a two-stage modelEarth and Planetary Science Letters, 26
M. Esfahani, M. Khalili, N. Kochhar, L. Gupta (2010)
A-type granite of the Hasan Robat area (NW of Isfahan, Iran) and its tectonic significanceJournal of Asian Earth Sciences, 37
M. Alavi (1994)
the Zagros erogenic belt of Iran: data and interpretations
Fukun Chen, W. Siebel, M. Satır (2002)
Zircon U–Pb and Pb-isotope fractionation during stepwise HF acid leaching and geochronological implicationsChemical Geology, 191
K. Ludwig (2003)
User's Manual for Isoplot 3.00 - A Geochronological Toolkit for Microsoft Excel
R. Batchelor, P. Bowden (1985)
Petrogenetic interpretation of granitoid rock series using multicationic parametersChemical Geology, 48
Liangshang Zhang, U. Schärer (1996)
Inherited Pb components in magmatic titanite and their consequence for the interpretation of UPb agesEarth and Planetary Science Letters, 138
Ranin Ahmad, Sepahi Asghar, Moinvaziri Hossein, Aliani Farhad (2010)
PETROLOGY AND GEOCHEMISTRY OF THE PLUTONIC COMPLEXES OF THE MARIVAN AREA, SANANDAJ-SIRJAN ZONEPetrology, 1
A. Baharifar, H. Moinevaziri, H. Bellon, A. Piqué (2004)
THE CRYSTALLINE COMPLEXES OF HAMADAN (SANANDAJ-SIRJAN ZONE, WESTERN IRAN): METASEDIMENTARY MESOZOIC SEQUENCES AFFECTED BY LATE CRETACEOUS TECTONO-METAMORPHIC AND PLUTONIC EVENTSComptes Rendus Geoscience, 336
KR Ludwig (1988)
Pbdat for MS-Dos — a computer program for IBM-PC compatibles for processing raw Pb-U-Th isotope data
(2013)
Petrology, Isfahan University, Iran
(2009)
Petrogensis of plutonic bodies and metamorphic rocks in the Marivan area
M. Arvin, Yuanming Pan, S. Dargahi, A. Malekizadeh, A. Babaei (2007)
Petrochemistry of the Siah-Kuh granitoid stock southwest of Kerman, Iran: Implications for initiation of Neotethys subductionJournal of Asian Earth Sciences, 30
KR Ludwig (2003)
Isoplot 3.0: a geochronological toolkit for Microsoft Excel vol. 4. Berkeley Geochronology Center, Special Publication 4
S. Alirezaei, J. Hassanzadeh (2012)
Geochemistry and zircon geochronology of the Permian A-type Hasanrobat granite, Sanandaj–Sirjan belt: A new record of the Gondwana break-up in IranLithos, 151
S. Mahmoudi, F. Corfu, F. Masoudi, B. Mehrabi, M. Mohajjel (2011)
U–Pb dating and emplacement history of granitoid plutons in the northern Sanandaj–Sirjan Zone, IranJournal of Asian Earth Sciences, 41
H. Shahbazi, W. Siebel, M. Pourmoafee, M. Ghorbani, A. Sepahi, C. Shang, M. Abedini (2010)
Geochemistry and U-Pb zircon geochronology of the Alvand plutonic complex in Sanandaj-Sirjan Zone (Iran): New evidence for Jurassic magmatismJournal of Asian Earth Sciences, 39
B. Frost, Calvin Barnes, W. Collins, R. Arculus, D. Ellis, C. Frost (2001)
A Geochemical Classification for Granitic RocksJournal of Petrology, 42
K. Ludwig (1988)
PBDAT for MS-DOS; a computer program for IBM-PC compatibles for processing raw Pb-U-Th isotope data, version 1.00a
F Masoudi (1997)
Contact metamorphism and pegmatites development in the region SW of Arak, Iran
J. Pearce, N. Harris, A. Tindle (1984)
Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic RocksJournal of Petrology, 25
R. Pidgeon, D. Bosch, O. Bruguier (1996)
Inherited zircon and titanite UPb systems in an Archaean syenite from southwestern Australia: implications for UPb stability of titaniteEarth and Planetary Science Letters, 141
A. Esna-Ashari, M. Tiepolo, M. Valizadeh, J. Hassanzadeh, A. Sepahi (2011)
Geochemistry and zircon U–Pb geochronology of Aligoodarz granitoid complex, Sanandaj-Sirjan Zone, IranJournal of Asian Earth Sciences, 43
AA Baharifar (2004)
Petrology of metamorphic rocks in the Hamadan area
M. Moazzen, M. Moayyed, Monir Modjarrad, Esmail Darvishi (2004)
Azna granitoid as an example of syn-collision S-type granitisation in Sanandaj-Sirjan metamorphic belt, IranNeues Jahrbuch Fur Mineralogie-monatshefte, 2004
H. Azizi, Y. Asahara, B. Mehrabi, Sun‐Lin Chung (2011)
Geochronological and geochemical constraints on the petrogenesis of high-K granite from the Suffi abad area, Sanandaj-Sirjan Zone, NW IranChemie Der Erde-geochemistry, 71
M. Alavi (2004)
Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolutionAmerican Journal of Science, 304
Abstract 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 ancient active continental margin of the Neo-Tethyan ocean at the southeastern edge of the central Iranian 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 climax 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 magmatic 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.
Geochronometria – de Gruyter
Published: Sep 1, 2014
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