[1] Jamieson R. A., "PT paths from high temperature shear zones beneath ophiolites", Journal of Metamorphic Geology 4 (1986) 3-22.
[3] John T., Scherer E. E., Schenk V., Herms P., Halama R., Garbe-Schönberg, D., "Subducted seamounts in an eclogite-facies ophiolite sequence: The Andean Raspas Complex, SW Ecuador". Contributions to Mineralogy and Petrology 159 (2010) 265-284.
[4] Azizi H., Moinevaziri H., Mohajjel M., Yagobpoor A., “P-T path in metamorphic rocks of Khoy region (northwest Iran) and their tectonic significance for Cretaceous-Tertiary continental collision”, Journal of Asian Earth Siences 27 (2006) 1-9.
[5] Faridazad M., Moayyed M., Modjtahedi M., Moazzen M., “Petrology and petrogenesis of Amphibolitic rocks of the Khoy ophiolitic complex- NW Iran”, Iranian Journal of Crystallography and Mineralogy 18 (2) (2010) 233-246.
[6] Moazzen M., “Protolith nature and tectonomagmatic features of amphibolites from the Qushchi Area, West Azerbaijan, NW Iran” Bulletin of The Mineral Research and Exploration 149 (2014) 139-152.
[7] Hajialioghli R., Fakharinezhad H., Moazzen M., “Petrology and geochemistry of amphibolites from southeast of Siyah- Cheshmeh, NW Iran” Geosciences 25 (2016) 111-122.
[8] Azizi H., Chung S. L., Tanaka T., Asahara Y., “Isotopic dating of the Khoy metamorphic complex (KMC), northwestern Iran: A significant revision of the formation age and magma source”, Precambrian Research 185 (3) (2011) 87-94.
[9] Khodabandeh A. A., Soltanni G. A., Sartipi A. H., Emami M. H., “Geological map of Iran, 1: 100,000 series sheet Salmas”, Geological Survey of Iran, Tehran (2002).
[10] Stöcklin J., "Structural history and tectonics of Iran: A review", American Association Petroleum Geologists 52 (1968) 1229-1258.
[11] Homke S., Vergés J., Garcés M., Emami H., Karpuz R., "
Magnetostratigraphy of Miocene–Pliocene Zagros foreland deposits in the front of the Push-e Kush arc (Lurestan Province, Iran)", Earth Planet. Sci. Lett. 225(2004). https:
// doi.org.
10.1111/j.1365-2117.2009.00431.x
[12] Mouthereau F., Lacombe O., Vergés J., "
Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence". Tectonophysics, 532-535 (2012) 27-60.
10.1016/j.tecto.2012.01.022
[13] Hassanzadeh J., Wernicke B. P., “
The Neotethyan Sanandaj-Sirjan zone of Iran as an archetype for passive margin-arc transitions”, Tectonics
35(2016) 586-621. https:
// doi.org.
10.1002/2015TC003926.
[14] Alavi, M.A. “Structures of the Zagros Fold-Thrust Belt in Iran”, American Journal of Science, 307(2007)1064-1095. http://dx.doi.org/10.2475/09.2007.02
[15] Agard P., Omrani J., Jolivet L., Mouthereau F., “Convergence history across Zagros (Iran): Constraints from collisional and earlier deformation”, International Journal of Earth Science 94 (2005) 401- 419. https://doi.org/10.1007/s00531-005-0481-4.
[17] Robertson A.H.F., “Overview of tectonic settings related to the rifting and opening of Mesozoic ocean basins in the Eastern Tethys: Oman, Himalayas and Eastern Mediterranean regions”, Geological Society, London, Special Publications, 282/1 (2007) 325-389.
[18] Agard P., Jolivet L., Vrielynck E. Burov B., Monié P., “Plate acceleration: The obduction trigger?”, Earth and Planetary Science Letters, 258 (2007) 428–441.
[19] Azizi H., Stern R. J., “
Jurassic igneous rocks of the central Sanandaj–Sirjan zone (Iran) mark a propagating continental rift, not a magmatic arc”, Terra Nova. 31 (2019) 415-423.
https://doi.org/10.1111/ter.12404
[20] Azizi H., Tsuboi M., “
The Van Microplate: A new microcontinent at the junction of Iran, Turkey, and Armenia”, Frontiers in Earth Science 8 (2021) Article 574385.
https://doi.org/10.3389/feart.2020.574385
[21] Shafaii Moghadam H., Griffin W.L., Kirchenbaur M., Garbe-Schönberg D., Zakie Khedr M., Kimura J, I., Stern R,J., Ghorbani Gh, Murphy R.,
O'Reilly S,Y., Arai Sh., Maghdour-Mashhour R., “
Roll-back, extension and mantleupwelling triggered Eocene potassic magmatism in NW Iran”, Journal of Petrology 59 (2018) 1417-1465.
https://doi.org/10.1093/petrology/egy067
[22] Allahyari K., Saccani E., Rahimzadeh B., Zeda O., “
Mineral chemistry and petrology of highly magnesian ultramafic cumulates from the Sarve-Abad (Sawlava) ophiolites (Kurdistan, NW Iran): New evidence for boninitic magmatism in intra-oceanic fore-arc setting in the Neo-Tethys between Arabia and Iran”, Journal of Asian Earth Sciences 79 (2014) 312-328.
https://doi.org/10.1016/j.jseaes.2013.10.005
[23] Saccani E., Allahyari K., Rahimzadeh B. “
Petrology and geochemistry of mafic magmatic rocks from the Sarve-Abad ophiolites (Kurdistan region, Iran): Evidence for interaction between MORB-type asthenosphere and OIB-type components in the southern Neo-Tethys Ocean”, Tectonophysics 621(2014) 132-147.
https://doi.org/10.1016/j.tecto.2014.02.011
[24] Rezaei M., Moazzen M., “
Mineral chemistry of the ophiolitic peridotites and gabbros from the Serow area: Implications for tectonic setting and locating the Neotethys suture in NW Iran”, Central European Geology 57(2014) 385-402.http:doi.org
/ 10.1556/CEuGeol.57.2014.4.4
[25]
Hajialioghli R., Moazzen M., “
Supra-subduction and mid-ocean ridge peridotites from the Piranshahr area, NW Iran”, Journal of Geodynamics 81 (2014) 41-55. https:
// doi.org.
10.1016/j.jog.2014.06.003
[27]
Shafaii Moghadam H., Li Li Q, Stern R.J.,
Chiaradia M.,
Karsli O.,
Rahimzadeh B., “
The Paleogene ophiolite conundrum of the Iran-Iraq border region”, Journal of the Geological Society 177 (2020) 955-964.
[28] Aswad K.J.A., Aziz N.R.H., Koyi H.A. “Cr-spinel compositions in serpentinites and their implications for the petrotectonic history of the Zagros Suture Zone, Kurdistan Region, Iraq”, Geol. Mag. 148 (2011) 802-818.
[29] Ali S.A., Buckman S., Aswad K.J., Jones B.G., Ismail S.A., Nutman A., “
The tectonic evolution of a Neo-Tethyan (Eocene–Oligocene) island‐arc (Walash and Naopurdan groups) in the Kurdistan region of the northeast Iraqi Zagros Suture Zone”, Island Arc 22 (2013)104-125. https:
// doi.org/10.1111/iar.12007
[30] Ali S. A., Ismail S. A., Nutman A. P., Bennett V. C., Jones B. G., Buckman S., “The intra oceanic Cretaceous (∼108 Ma) Kata-Rash arc fragment in the Kurdistan segment of Iraqi Zagros Suture Zone: Implications for Neotethys evolution and closure”, Lithos 260 (2016) 154-163.
[31] Allahyari K., Saccani E., Pourmoafi M., Beccaluva L., Masoudi F., “
Petrology of mantle peridotites and intrusive mafic rocks from the Kermanshah ophiolitic complex (Zagros belt, Iran): Implications for the geodynamic evolution of the Neo-Tethyan oceanic branch between Arabia and Iran”, Ofioliti, 35 (2010) 71-90.
https://doi.org/10.4454/ofioliti.v35i2.387
[32] Alavi M., “Etude geologique de la region de Djam”, Geological Survey of Iran, Report, 23 (1972):1-288.
[34] Khalatbari-Jafari M., Jutea T., Bellon H., Whitechurch H., Cotton J., Emami H., “New geological, geochronological and geochemical investigation on the Khoy ophiolites and related formations”, NW Iran. Journal of Asian Earth Sciences 23(2004) 507-535.
[35] Hajmolla Ali E., Shahrabi M., Tahooneh M., Shokri S., “Silvana, geological quadrangle map, 1:100000 scale”, Geological Survey of Iran, Tehran (2006).
[36] Arabshahi A. H., Sabzeie M., “Geological 1:25000 map of Silvaneh”, Geological Survey of Iran. Tehran (2013).
[37] Whitney D., Evans B., “Abbreviations for names of rock-forming minerals”, American Mineralogist. 95 (2010) 185-187.
[38] Pearce J.A., Stern R.J., “
Origin of Back-Arc Basin Magmas: Trace Element and Isotope Perspectives”, In: Christie, D.M., Fisher, C.R., Lee, S.M. and Givens, S., Eds., Back-Arc Spreading Systems; Geological, Biological, Chemical, and Physical Interactions. Geophysical Monograph Series 166, American Geophysical Union, Washington (2006) 63-86.
http://dx.doi.org/10.1029/166gm06
[39] Best M. G., “Igneous and metamorphic petrology”, W. H. Freeman and Co., San Francisco 2 (1982): 1-630.
[40] Kocak K., Kurt H., Veysel Z. Ferré E.C., “Characteristic of the amphibolites from nigde metamorphic (Central Turkey), deduced from whole rock and mineral chemistry”, Geochemical Journal 41 (2007) 241-257.
[41] Garrels R.M. Mackenzie F.T., “Evolution of sedimentary rocks”, W. W. Norton and Company, Inc., New York (1971) 397p.
[42] Pearce J.A., “A user‘s guide to basalt discrimination diagrams. Trace element geochemistry of volcanic rocks: Applications for massive sulphide exploration”, Geological Association of Canada, Short Course Notes, 12 (1996) 79-113.
[43] Winchester J. A., Floyd P.A., "Geochemical magma type discrimination: Application to altered and metamorphosed igneous rocks", Earth and Planetary Science Letters 28 (1976) 459-469.
[44] Miyashiro A., “Volcanic rock series in island arcs and active continental margins”, American Journal of Science 274 (1974) 321-355.
[45] Ross P.S., Bédard J.H., “
Magmatic affinity of modern and ancient subalkaline volcanic rocks determined from trace-element discriminant diagrams”, Canadian Journal of Earth Sciences 46 (2009) 823-839.
https://doi.org/10.1139/E09-054
[47] Sun S. S., McDonough W. F.,
"Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes", In: Saunders A. D., Norry M. J. (Eds.), Magmatism in Ocean Basins", Special Publications, Geological Society, London 42 (1989) 312-345.
[48] Eyuboglu Y., Santosh M., Bektas O., Ayhan S., "Arc magmatism as a window to plate kinematics and subduction polarity", Example from the eastern Pontides belt, NE Turkey. Geoscience Frontiers. 2 (2011) 49-56. https://doi.org/10.1016/j.gsf.2010.12.004
[49] Srivastava R.K., Chandra R., Shastry A., “High-Ti type N-MORB arentage of basalts from the south Andaman ophiolite suite, India”, Proc. Indian Acad. Sci. (Earth Planet. Sci), 113, no. 4, December 2004, pp. 605-618.
[50] O’Neill H. St. C., “The transition between spinel lherzolite and garnet lherzolite and its use as a geobarometer”, Contributions to Mineralogy and Petrology 77 (1981) 185-194, https://doi.org/10.1007/BF00636522
[51] Juteau T., Maury R., “The oceanic crust, from accretion to mantle recycling”, Springer-Praxis, Chichester, UK (1999) 390p.
[53] Kuster D., Harms U., “Post-collisional potassic granitoids from the southern and northwestern parts of the Late Neoproterozoic East African orogen: A review”, Lithos 45 (1998) 177-195.
[54] Ishikawa A., Kaneko Y., Kadarusman A., Ota T., “Multiple generations of forearc mafic–ultramafic rocks in the Timor–Tanimbar ophiolite, eastern Indonesia”, Gondwana Research 11(2007) 200-217. doi:10.1016/j.gr.2006.04.007.
[55] Reagan M.K., Ishizuka O., Stern R.J., Kelley K.A., Ohara Y., Blichert-Toft J., Bloomer S.H., Cash J., Fryer P., Hanan B.B., Hickey-Vargas R.,
“Fore-arc basalts andsubduction initiation in the Izu-Bonin-Mariana system”, Geochem. Geophys.Geosys 11 (2010), Q03X12.
https://doi.org/10.1029/2009GC00287
[56] Shervais J.W., Reagan M.K., Haugen E., Almeev R., Pearce J.A., Prytulak J., Ryan J.G., Whattam S.A., Godard M., Chapman T., Li H.Y., Kurz W., Nelson W.R., Heaton, Kirchenbaur M., Shimizu K., Sakuyama T., Li Y., Vetter S.K, “Magmatic Response to Subduction Initiation, Part I: Fore-arc basalts of the Izu-Bonin Arc from IODP Expedition 352”, Geochem. Geophys. Geosys 20 (2019) 314-338. https://doi.org/10.1029/2018GC007731.
[57] Stern R.J., Lin P.N., Morris J.D., Jacson M.C., Fryer P., Bloomer S.H., Ito E., “Enriched back-arc basin basalts from the northen Mariana trough: Implictions for the magmatic evolution of back-arc basin”, Earth Planet Science Letter 210 (1990) 481-497.
[58] Frenzel G., Muhe R., Stoffers P., “Petrology volcanic rocks from the Lau basin, South West pacific”, Geol, Jb., 22 (1990) 395-479.
[59] Dilek Y., Flower M.F.j., “Arc-trench rollback and forearc accretion. 2. A model template for ophiolites in Albania, Cyprus, and Oman”, Geological Society, London, Special Publications 218 (2003) 43-68.
[60] Beccaluva L., Coltorti M., Giunta G., Siena F., “Tethyan vs. Cordilleran ophiolites: a reappraisal of distinctive tectono-magmatic features of suprasubduction complexes in relation to the subduction mode”, Tectonophysics 393 (2004) 163-174.
[62] Pearce J.A., Gale G.H., “Identification of ore-deposition environment from trace element geochemistry of associated igneous host rock”, Geol. Soc. Spec. Publ., 7 (1977) 14-24.
[63] Mullen E.D., “
MnO/TiO2/P2O5: A minor element discriminant for basaltic rocks of oceanic environments and its implications for petrogenesis”, Earth and Planetary Science Letters 62 (1983) 53-62,
https://doi.org/10.1016/0012-821X(83)90070-5.
[64] Shervais J. W., "Ti-V plots and the petrogenesis of modern and ophiolitic lavas", Earth and Planetary Science Letters 59 (1982) 101-118.
[65] Yaliniz M.K., “A geochemical attempt to distinguish forearc and backarc ophiolites from the supra- subduction Central Anatolian ophiolites (Turkey) by comparison with modern oceanic analogues”, Ofioliti 33 (2008) 119- 129.
[66] Pearce J. A., Norry M. J., “Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks”, Contributions to Mineralogy and Petrology 69 (1979) 33-47.
[67] Sommer C. A., Lima E. F., Nardi L.V.S., Liz J.D., Waichel B.L., “The evolution of Neoproterozoic magmatism in Southernmost Brazil: shoshonitic, high- K tholeiitic and silica- saturated, sodic alkaline volcanism in post collisional basins”, Anais da Academia Brasileira de Ciencias 78 (2006) 573- 589.
[68] Muller D., Groves D.I., “Potassic igneous rocks and associated gold-copper mineralization”, Springer-Verlag, Berlin, Heidelberg, 238 p (1997).
[70] Pearce J.A., “Trace element characteristics of lavas from destructive plate boundaries”, In Andesites, edited by J. S. Thorpe (1982) 525–548, John Wiley, New York.
[71] Woodhead J., Eggins S., Gamble J., ”High field strength and transition element systematics in island arc and back-arc basin basalts: evidence for multi-phase melt extraction and a depleted mantle wedge”, Earth and Planetary Science Letters 114 (1993) 491-504.
[72] Tatsumi Y., Kogiso T. Nohda S., “Formation of a third volcanic chain in Kamchatka: Generation of unusual subduction-related magmas”, Contributions to Mineralogy and Petrology 120 (1995) 117-128, https://doi.org/10.1007/BF00287109.
[73] Wilson M., “Igneous Petrogenesis: A global tectonic approach”, Unwin Hyman, London (1989) 466p.
[74] Schmincke U., “Volcanism”, Springer, Verlag, Berlin Heidelberg New York (2004) 324p.
[75] Suda Y., Hayasaka Y., Kimura K., “Crustal evolution of a Paleozoic intra-oceanic island-arc-back-arc basin system constrained by the geochemistry and geochronology of the Yakuno ophiolite, southwest Japan”, Journal of Geological Research 5(2014) 1-10, http://dx.doi.org/10.1155/2014/652484.
[76] Conly A. G., Bernan J. M., Bellon H. Scott S. D., “Arc to rift transitional volcanism in the Sanata Rosalia Region, Baja California Sur, Maxico”, Journal of Geology 72 (2005) 303-341.
[77] Beier C., Brandl P. A., Lima S. L., Haase K. M., “Tectonic control on the genesis of magmas in the New Hebrides arc (Vanuatu)”, Lithos 312-313 (2018), 290-307.
[78] Pearce J. A., ”Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust”, Lithos, 100 (2008) 14-48.
[79] Whattam S.A., Stern R.J., “The subduction initiation rule: A key for linking ophiolites, intra-oceanic forearcs, and subduction initiation”, Contributions to Mineralogy and Petrology 162 (2011) 1031-1045, https:// doi .org /10 .1007 /s00410 -011 -0638-z.
[80] Pearce J. A., Peate D. W., “Tectonic implications of the composition of volcanic arc magmas”, in Wetherill, G., Albee, A., and Burke, K., editors, Annual Review of Earth and Planetary Sciences: Palo Alto, Annual Reviews 23 (1995) 251-285. http://dx.doi.org/10.1146/annurev.ea.23.050195.001343
[81] Yang Q.Y., Santosh M., Shen J.F., Li S.R., “Juvenile vs. recycled crustin NE China: Zircon U-
Pb geochronology, Hf isotope and integrated model for Mesozoic gold mineralization in the Jiadong Peninsula”, Gondwana Research, 25(2014): 1445–1468. https://doi.org/10.1016/j.gr.2013.06.003
[82] Zhao J.J., Zhou M.F., “Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua district (Sichuan Province, SW China): implications for subduction-related metasomatism in the upper mantle”, Precambrian Research, 152(2007) 27-47.
https://doi.org/10.1016/j.precamres.2006.09.002
[83] Zhu C. Y., Zhao G., Sun M., Eizenhöfer P. R., Liu Q., Zhang X., Han, Y., Hou W., “Geochronology and geochemistry of the Yilan greenschists and amphibolites in the Heilongjiang complex, northeastern China and tectonic implications”, Journal of Gondwana Research 43 (2017) 213-228.
)