[1] Berberian M., King G.C.P., “Towards a paleogeography and tectonic evolution of Iran”, Canadian Journal of Earth sciences 18 (1981) 210-265.
[2] Segnӧr A.M.C., “A new model for the late Paleozoic-Mesozoic tectonic evolution of Iran and imlications for Oman. In: Robertson, A.H.F., Searle, M.P., Ries, A.C. (Eds), The Geology and Tectonics of the Oman region”, Geological Society, London, Special Publication 49, pp. (1990) 797-831.
[3] Alavi M., “Tectonostratigraphic synthesis and structural style of the Alborz Mountain System in Iran”, Journal of Geodynamics, 21(1) (1996) 1–33
[4] Brunet M.F., Granath J.W., Wilmsen M., “South Caspian to Central Iran Basins: Introduction”, Geological Society, London, 312 (2009) 1-6
[5] Stӧcklin J., “Structural history and tectonics of Iran: a review”, The American Association of petroleum Geologists Bulleti, USA, 52 (7) (1968) 1229-1258
[6] Alric G., Virlogeus D., “Petrography and Geochemistry study of metamorphic and magmatic in Dehbid-Bavanat Region”, Report 21, Geological Survey of Iran (1977).
[7] Emami M.E., “Magmatism in Iran”, Geological and Mineral Exploration Organization of the country (2000). (in Persian).
[8] Hooshmandzadeh A., Soheili M., Owhanian T., Sahandi M., Azarm F., “Explanatory text of the Eqlid quadrangle geological map”, scale 1:250,000. Geological Survey of Iran. (1990). (in Persian).
[9] Azizi H., Stern R.,
“Jurassic igneous rocks of the central Sanandaj-Sirjan Zone (Iran) mark a propagating continental rift”, not a magmatic arc. Terra Nova, 31(5) (2019) 415-423. DOI:
10.1007/s00531-005-0481-4
[10] Sheikholeslami M. R., “Tectonostratigraphic units of southeastern part of the Sanandaj–Sirjan zone”, Scientific Quarterly Journal of Geosciences, 24(95) (2015) 243–253.
[11] Harrison J. V., Falcon N. L., Archer R., “The geology of the Kuh-i-Nur district (southern slopes of the central Elburz Mountains, Persia)”, Geological Magazine, 73(12) (1936) 529–552.
[12] Moradian E., Shabanian N., Davodian A., Azizi H., “Mineral assemblage and metamorphic evolution of metasediments and metabasites in the Tutak Complex, Southeastern Bavanat, Fars Province”, Journal of Iranian Crystallography and Mineralogy, 31(1) (2023) 91-104 (in Persian).
[13] Bendokht M., Shabanian N., Davoudian A. R., Dong Y., Cottle J. M., Johnson T. A.,
“Geochronology and geochemistry of Cadomian basement orthogneisses from the Tutak metamorphic Complex, Sanandaj-Sirjan Zone”, Iran. Precambrian Research, 362 (2021) 106288.
https://doi.org/10.1016/j.precamres.
[14] Hosseini B., Ahmadi A., Ghorbani M., “Metamorphic evolution of the Toutak complex (Sanandaj-Sirjan Zone, Iran)”, Geophysical Research Abstracts, 11 (2009) EGU2009-1077.
[15] Bendokht M., Davoudian A. R., Sari S., Kuru S., Sevcan Kuru, "Zircon U–Pb Geochronology and Lu–Hf Isotope Geochemistry Constraints on Neoproterozoic S-Type Meta-Granites from the Tutak Area, Sanandaj–Sirjan Zone, Iran", Lithos 438 (2023) 106998.
https://doi.org/10.1016/j.lithos.2022.106998.
[16] Rajabzadeh M., Rasti S., “Mineralization study of the Dehbid magnetite deposit, Fars Province, using mineralogical and geochemical data”, Economic Geology Journal of Iran, 3(2) (2011) 217–230.
[17] Taraz H., “Geological de la region de Surmaq-Deh-Bid (Iran central) – These doct”, detat-Paris-Sud-Orsay(1972).
[18] Taraz H., “Geology Of The Surmaq-Deh Bid Area Abadeh Region, Central Iran”, Ministry of Industry and Mines. Geological Survey of Iran no. 37 (1974).
[19] Bonyadi Z., Ghorbani S., “(n.d.). Mineralogical studies of the iron–manganese deposit of Heneshk, Fars Province. [Unpublished conference paper], Department of Geology, Imam Khomeini International University; Mining Unit”, Fili Investment Holding. (2015)
[20] Spitz G., Darling R.,
“Major and minor element lithogeochemical anomalies surrounding the Louvem copper deposit, Val d’Or, Quebec. Can”, J. Earth Sci. 15 (1978) 1161–1169.
https://doi.org/10.1139/e78-122.
[21] Le Bas M.J., Le Maitre R.W., Streckeisen A., Zanettin B., “A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram”, Journal of Petrology, 27 (1986) 745-750.
[22] Winchester J. A., Floyd P. A., “Geochemical discrimination of different magma series and their differentiation products using immobile elements”, Chem. Geol., 20, 235-343.
[23] Hastie A. R., Kerr A. C., Pearce J. A., Mitchell S. F.,
“Classification of altered volcanic island arc rocks using immobile trace elements: Development of the Th-Co discrimination diagram”, Journal of Petrology, 48(12) (2007) 2341–2357.
https://doi.org/10.1093/petrology/egm062
[24] Shand S. J., “Eruptive rocks: Their genesis, composition, classification, and their relation to ore-deposits”, London: Murby. (1947).
[25] Frost B. R., Barnes C. G., Collins W. J., Arculus R. J., Ellis D. J., Frost C. D., “A geochemical classification for granitic rocks”, Journal of Petrology, 42(11) (2001) 2033–2048.
[26] Chappell B. W., White A. J. R., “I- and S-type granites in the Lachlan Fold Belt. Transactions of the Royal Society of Edinburgh”, Earth Sciences, 83(1–2) (1992) 1–26.
[27] Nabelek Peter I., Mingming L., “Petrologic and thermal constraints on the origin of leucogranites in collisional orogens”, Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 95(1–2) (2004) 73–85. DOI: 10.1017/S0263593300000916
[28] Harker A., “The Natural History of Igneous Rocks”, Methuen, London. (1909) 348p.
[29] Sun S.S., McDonough W.F., “Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes”, Geol. Soc. Lond. Spec. Publ., 42 (1989) 313-34 https :// doi.org/ 10.1144/GSL .SP. 1989 .042.01.19
[30] Rollinson H. R., “Using geochemical data: Evaluation, presentation, interpretation”, Longman, Harlow. (1993).
[31] Prowatke S., Klemme S., “Trace element partitioning between apatite and silicate melts”, Geochimica et Cosmochimica Acta, 70(17) (2006) 4513–4527. https://doi.org/10.1016/j.gca.2006.07.010
[32] Yakymchuk C., “Behaviour of apatite, monazite, zircon, and xenotime during metamorphism”, Geological Society, London, Special Publications, 449(1) (2017) 215–235.
[33] Taylor S.R., McLennan S.M., “The geochemical evolution of the continental crust”, Review Geophysics, 33 (1995) 241-265. doi:10.1029/95RG00262
[34] Randive B., San Sebastian M., De Costa A., Lindholm L., “Inequalities in institutional delivery uptake and maternal mortality reduction in the context of cash incentive program, Janani Suraksha Yojana: Results from nine states in India”, Social Science & Medicine, 123 (2014) 1–6. https://doi.org/10.1016/j.socscimed.2014.10.042
[37] Defant M.J., Drummond M.S.,
“Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere”, Nature, 347 (1990) 662-665.
https://doi.org/10.1038/347662a0
[38] Moyen J.F., Laurent O., Chelle-Michou C., Couzini´e S., Vanderhaeghe O., Zeh A., Villaros A., Gardien V., “Collision vs. subduction-related magmatism: two contrasting ways of granite formation and implications for crustal growth”, Lithos 277 (2017) 154–177. https://doi.org/10.1016/j.lithos.2016.09.018.
[39] McDonough W.F., Sun S.S., “The Composition of the Earth”, Chemical Geology, 120 (1995) 223-253.
https://doi.org/10.1016/0009-2541(94)00140-4
[40] Rudnick R.L., “Making continental crust”, Nature, 378 (1995) 571-578, https://doi.org/10.1038/378571a0,
[41] Weyer S., Muenker C., Mezger K., “Nb/Ta, Zr/Hf and REE in the depleted mantle: implications for the differentiation history of the crust-mantle system, Earth Planet”, Sc. Lett, 205 (2003) 309-324, https://doi.org/10.1016/S0012-821X(02)01059 2,
[42] Wilson M., “Igneous Petrogenesis: A Global Tectonic Approach”, Unwin Hyman, London, 466 p. (1989)
https://doi.org/10.1007/978-1-4020-6788-4
[43] Frey F. A., Green D. H., Roy S. D.,
“Integrated Models of Basalt Petrogenesis: A Study of Quartz Tholéiites to Olivine Melilitites from South Eastern Australia Utilizing Geochemical and Experimental Petrological Data”, Journal of Petrology, 19 (1978) 463-513.
https://doi.org/10.1093/petrology/19.3.463
[44] Rapp R. P., Watson E. B., “Dehydration melting of metabasalt at 8–32 kbar: Implications for continental growth and crust–mantle recycling”, J. Petrol., 36 (1995) 891-931, https://doi.org/10.1093/petrology/36.4.891
[45] Hawkesworth C. J., Kemp A. I. S., “The differentiation and rates of generation of the continental crust”, Chem. Geol., 226 (2006) 134-143.
https://doi.org/10.1016/j.chemgeo.2005.09.017, 2006.
[47] Jaupart C., Mareschal J. C., “Heat Flow and Thermal Structure of the Lithosphere. In: Schubert, G., Ed., Treatise on Geophysics”, Elsevier, Oxford, (2007) 217-252.
https://doi.org/10.1016/B978-044452748-6.00104-8
[48] Rudnick R. L., Barth M., Horn I., McDonough W. F., “Rutile-bearing refractory eclogites: Missing link between continents and depleted mantle”, Science, 281(5379) (1998) 1841–1844. doi: 10.1126/science.287.5451.278.
[49] Rudnick R.L., Gao S., “Composition of the continental crust”, Treatise On Geochemistry, 3: 1–64. (2003) doi:10.1016/0016-7037(95)00038-2.
[50] Regelous A., Scharfenberg L., De Wall H., “Origin of S-, A- and I-type granites: petrogenetic evidence from whole rock Th/U ratio variations”, Minerals 11 (2021) 672.
[51] Boztuğ D., Harlavan Y., Arehart G.B., Satir M., Avci N., “K-Ar age, whole-rock and isotope geochemistry of A-type granitoids in the Divriği-Sivas region, eastern-central Anatolia, Turkey”, Lithos, 97, 193-218, https://doi.org/10.1016/j.lithos.2006.12.014, 2007.
[52] Clarke D.B., “Granitoid rocks. Chapman & Hall”, London, 283 pp. (1992)
[53] Yang J. H., Wu F. Y., Wilde S. A., Xie L. W., Yang Y. N., Liu X. M., “Petrogenesis of an Early Cretaceous granite from the North China Craton: In situ Hf isotopic evidence for remelting of ancient lower crust”, Journal of Asian Earth Sciences, 32(1) (2008) 1–11.
[54] Sylvester P.J., “Post-Collisional Strongly Peraluminous Granites”, Lithos, 45 (1998) 29-44.
https://doi.org/10.1016/S0024-4937(98)00024-3
[55] Blevin P.L., “Redox and Compositional Parameters for Interpreting the Granitoid Metallogeny of Eastern Australia: Implications for Gold-Rich Ore Systems”, Resource Geology, 54 (2004) 241-252.
https://doi.org/10.1111/j.1751-3928.2004.tb00205.x
[56] Harris N., Inger S., Massey J., “The role of fluids in the formation of High Himalayanleucogranites. In Himalayan Tectonics. Edited by P.J. Treloar, and M.P. Searle”, Geological Society, London, Special Publication, No. 74 (1993) pp. 391–400..
[57] Watson E. B., Harrison T. M., “Zircon saturation revisited: Temperature and composition effects in a variety of crustal magma types”, Earth and Planetary Science Letters, 64(2) (1983) 295–304.
[58] Boehnke P., Watson E.B., Trail D., Harrison T.M., Schmitt A.K., “Zircon saturation Re-revisited”, Chemical Geology, 351 (2013) 324-334.https://doi.org/10.1016/j.chemgeo.2013.05.028
[59] Yang X.M., “Estimation of crystallization pressure of granite intrusions”, Lithos, 286–287 (2017) 324–329. doi:10.1016/j.lithos.2017.06.018.
[60] Tuttle O. F., Bowen N. L., “Origin of granite in the light of experimental studies in the system NaAlSi₃O₈–KAlSi₃O₈–SiO₂–H₂O”, Geological Society of America Memoir, 74, (1958) 153 p.
[61] Pearce J.A., Harris N.B.W., Tindle A.G., “Trace element discrimination diagrams for the tectonic interpretation of granitic rocks”, J. Petrol. 25 (1984) 956–983.
https://doi. org/10.1093/petrology/25.4.956.
[62] Harris N. B. W., Pearce J. A., Tindle A. G., “Geochemical characteristics of collision-zone magmatism”, In M. P. Coward & A. C. Ries (Eds.), Collision Tectonics (Vol. 19 (1986) pp. 67–81). Geological Society, London, Special Publications. https://doi.org/10.1144/GSL.SP.1986.019.01.04
[63] Pearce N.J.G., “Zirconium and niobium bearing ilmenites from the Igaliko Dyke Swarm”, South Greenland. (1990)
[64] Schandl E. S., Gorton M. P., “Application of High Field Strength Elements to Discriminate Tectonic Settings in VMS Environments”, Economic Geology, 97 (2002) 629-642.https://doi.org/10.2113/gsecongeo.97.3.629
[65] Batchelor R. A., Bowden P., “Petrogenetic interpretation of granitoid rock series using multicationic parameters”, Chemical Geology, 48(1–4) (1985) 43–55.
https://doi.org/10.1016/0009-2541(85)90034-8
[66] Brown M., “Granite: From genesis to emplacement”, Geological Society of America Bulletin, 125(7–8) (2013) 1079–1113. https://doi.org/10.1130/B30754.1
[67] Hildebrand R.S., Whalen J.B., Bowring S.A., “Resolving the crustal composition paradox by 3.8 billion years of slab failure magmatism and collisional recycling of continental crust”, Tectonophysics, 734–735 (2018) 69–88. doi:10.1016/j.tecto.2018.04.001
[68] Brown M., “Melting of the continental crust during orogenesis :the thermal, rheological, and compositional consequences of melt transport from lower to upper continental crust”, Canadian Journal of Earth Sciences, 47 (2010) 655–694. doi:10.1139/E09-057.
[69] Gao P., Zheng Y. F., Zhao Z. F., “Experiment almelts from crustal rocks: A lithochemical constraint on granite petrogenesis”, Lithos, 266–267 (2016) 133 157. doi:10.1016/j.lithos.2016.10.005.
[71] Polat A., Appel P. W. U., Frei R., “Trace element systematics of the Archean greenstone belts: Implications for tectonic setting”, Precambrian Research, 261 (2015) 1–21.
[72] Polat A., Kokfelt T., Burke K.C., Kusky T.M., Bradley D.C., Dziggel A., Kolb J., “Lithological, structural, and geochemical characteristics of the Mesoarchean Târtoq greenstone belt, southern West Greenland, and the Chugach–Prince William accretionary complex, southern Alaska: evidence for uniformitarian plate-tectonic processes”, Canadian Journal of Earth Sci ences, 53 (2016) 1336–1371. doi:10.1139/cjes-2016-0023.
[73] Hildebrand R. S., Whalen J. B.,
“The tectonic setting and origin of Cretaceous batholiths within the North American Cordillera: The case for slab failure magmatism and its significance for crustal growth”
, In Circum-Pacific tectonics. geologic evolution, and ore deposits (Vol. 532 (2017) pp. 171–190). Geological Society of America.
https://doi.org/10.1130/2017.2532