[1] Aghanabati S.A., “Geology of Iran. Ministry of Industries and Mines”, Organization of Geology and Exploration of Minerals (In Persian) (2004) 586 p.
[2] Berberian M., “Late Cretaceous and Early Miocene Andean-type plutonic activity in northern Makran and Central Iran”, Journal of the Geological Society, 139(5) (1982) 605–614.
[3] Emami M.H., “Magmatism in Iran. Geological Survey of Iran”, Tehran. Report 1 (2000) 608 pp.
[4] Alirezaei A., Arvin M., Dargahi S., “Adakite-like signature of porphyry granitoid stocks in the Meiduk and Parkam porphyry copper deposits, NE of Shahr-e-Babak, Kerman, Iran”, constrains on geochemistry. Ore Geology Reviews, 88 (2017) 370–383.
[5] Moayyed M., “Petrologic studies of Tertiary volcano- plutonic belt in Western Alborz- Azarbaijan, with a special focus on Hashtchin area, Iran. PhD dissertation (In persian)”, Shahid Beheshti University (2002) 328 p.
[6] Farhoudi G., “A comparison of Zagros geology to island arcs”, The Journal of Geology, 86(3) (1978) 323 -334.
[7] Shahabpour J., “Tectonic evolution of the orogenic belt in the region located between Kerman and Neyriz”, Journal of Asian Earth Sciences, 24(4) (2005) 405–417.
[8] Verdel C., Wemicke B.P., Hassanzadeh J., Guest B., “A Paleogene extensional arc flare-up in Iran”, Tectonics, 30 (3) (2011) TC3008.
[9] Ghorbani M. R., Graham I. T., Ghaderi M., “Oligocene-Miocene geodynamic evolution of the central part of Urumieh-Dokhtar Arc of Iran”, International Geology Review, 56(8) (2014) 1039-1050.
[10] Nabavi M.H., Haqipour A., Valeh S., “Geological map 1:250000 of Yazd”, Iran's Geological and Mineral Exploration Organization (In Persian) (1972).
[11] Sepidbar F., Mirnejad H., Ma C., Moghadam H.S., “Identification of Eocene-Oligocene magmatic pulses associated with flare-up in east Iran”, Timing and sources. Gondwana Research 57 (2018) 141-156.
[12] Alavi M., “Tectonostratigraphic synthesis and structural style of the AlborzMountain System in Iran”, Journal of Geodynamics 21/1 (1996) 1-33.
[13] Stocklin J., “Structural history and tectonics of Iran”, a review. AAPG Bulletin, 52 (1968) 1229– 1258.
[14] Javadi H., Moayyed M., Harati H., Topuz G., “Petrography, geochemistry and emplacement environment of sub volcanic intrusives in Mehriz rigion of Yazd”, Iranian journal of crystallography and mineralogy. A-10-701-1 (R1). (In Persian with English abstract) (2025).
[15] Whitney D.L., Evans B.W., “Abbreviations for names of rock -forming minerals”, American Mineralogist 95 (2010) 185–187.
[16] Winchester J.A., Floyd P.A., “Geochemical discrimination of different magma Series and their differentiation products, using immobile elements”, Chem Geol, 22 (1977) pp. 325-343.
[17] Jensen L.S., “A New Cation Plot for Classifying Subalkalic Volcanic Rocks”, Ontario Geological Survey Miscellaneous Paper 66 (1976).
[18] 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.
[19] McDonough W.F., Sun S.S., “The composition of the Earth”, Chem. Geol., 120, 223 – 253.
[20] Boynton W.V., “Cosmochemistry of the rare earth elements: meteorite studies. In: Henderson”, P. (Ed.), Rare Earth Element Geochemistry. Elsevier, Amsterdam, (1984) 63–114.
[21] Pearce J. A., Harris N. B. W., Tindle A. G.,
“Trace element discrimination diagrams for the tectonic interpretation of granitic rocks”, Journal of petrology 25 (1984) 956-983.
[22] Ionov D. A., Hofman A. W., “Nb-Ta-rich mantle amphiboles and micas implications for subduction-related metasomatic trace element fractionation”, Erth. Planet. Sci. Lett 131 (1995) 341-356.
[23] Ayers J.C., “Trace element modeling for aqueous fluid-peridotite inter action in the wedge of subduction zones”, Contributions to Mineralogy and Petrology 132 (1998) 390-404.
[24] Stalder R., Foley S. F., Brey G. P., Horn I., “Mineral-aqueous fluid partitioning of trace -Elements at 900-1200 ºc and 3-5.7 GPA: new experimental data for garnet, clinopyroxene, and rutile, and implications for mantle metasomatism”, Geochimica et Cosmochimica Acta 62 (1998) 1781-1801.
[25] Gill J., “Orogenic Andesites and Plate Tectonics. Minerals, Rocks and Mountains. Goldstein, R.H., Reynolds, T.J., 1994. Systematics of fluid inclusions in diagenetic minerals. Short Course 31, Society of Economic Paleontologists and Mineralogists, Tulsa (1981) 199 p.
[26] Hawkesworth C.J., Gallagher K., Hergt J.M., Mcdermoot F., “Trace element fractionation processes in the generation of island arc basahs”, Phil. Trans. Roy. Sot. London A342 (1993) 171-191.
[27] Brenan J.M., Shaw H.F., Phinney Ryerson D.L. F.J., “Rutileaqueous fluid partitioning of Nb, Ta, Hf, Zr, U and Th: implications for high field strength element depletions in island-arc basalts”, Earth Planet. Sci. Lett. 128 (1994) 327 – 339.
[28] Foley S.F., Barth M.G., Jenner G.A., “Rutile/melt partition coefficients for trace elements and an assessment of the influence of rutile on the trace element characteristics of subduction zone magmas”, Geochim. Cosmochim. Acta 64 (2000) 933 – 938.
[29] Hou Z.Q., Zhang H.R., Pan X.F., Yang Z.M., “Porphyry Cu(–Mo–Au) deposits related to melting of thickened mafic lower crust: examples from the eastern Tethyan metallogenic domain”, Ore Geology Reviews 39 (2011) 21–45.
[30] Jung S., Hffer E., Hoernes S., “Neo-Proterozoic rift-related syenites (North Damara Belt, Namibia): Geochemical and Nd-Sr-PB-O istope constraints for mantle sources and petrogenesis”, Lithos, 96 (2007) 415-435.
[31] Henderson P., “Rare earth element geochemistry”, Elsevier, Amsterdam (1984).
[32] Kamber B. S., Ewart A., Collerson K. D., Bruce M. C., McDonald G. D., “Fluid-mobile trace element constraints on the role of slab melting and implications for Archaean crustal growth models”, Contributions to Mineralogy and Petrology, 144 (2002) 38–56.
[33] Nagudi N., Koberl Ch., Kurat G., “Petrography and geochemistry of the sigo granite, Uganda and implications for origin”, Journal of African Earth Sciences 36 (2003) pp 1-14.
[34] Glenn A.G., "The influence of melt structure on trace element partitioning near the peridotite solidus", Contrib Mineral Petrol. 147 (2003) 511-527p.
[35] Rollinson H.R., “Using Geochemical Data: Evolution, Presentation, Interpretation”, Longman Scientific and Technical, England (1993).
[36] Wu F.Y., Jahn B.M., Wilde S.A, Lo C.H, Yui T.F., Lin Q., Ge W.C., Sun D.Y., “Higly fractionated I-type granites in NE China (I): Geochronology and petrogenrsis”, Lithos, 66 (2003) Pp 241-273.
[37] Machado A., Lima E.F., Chemale J.F., Morta D., Oteiza O., Almeida D.P.M., Figueiredo A.M.G., Alexandre F.M., Urrutia J.L., “Geochemistry constraints of Mesozoic-Cenozoic calc-alkaline magmatism in the south Shetland arc, Antarctica”, Journal of South American Earth Sciences, 18(3-4) (2005 (407-425.
[38] Pearce J. A., Bender J. F., De Long S. E., Kidd W. S. F., Low P. J., Guner Y., Saroglu F., Yilmaz Y., Moorbath S., Mitchel J. G., “Genesis of collision volcanism in eastern Anatolia”, Turkey. Journal of Volcanology and Geothermal Research 44(1-2) (1990) 189-229. DOI: 10.1016/0377 0273(90)90018-B.
[39] Ulmer P., “Partial melting in the mantle wedge - the role of H2O in the genesis of mantle derived arc- related magmas”, Physics of the Earth and Planetary Interiors 127 (2001) 215-232. DOI: 10,1017/CBO9781139164467.
[40] Aldanmaz E., Pearce J. A., Thirlwall M. F., Mitchell J. G., "Petrigenetic evolution of late Cenozoic, post collision volcanism in western Anatolia, Tirkey", Journal of volcanology and geothermal Reasearch, 102 (2000) 67-97.
[41] Ellam R. M., Cox K. G., “An interpretation of Karoo picrate basalts in terms of interaction between asthenospheric magmas and the mantle lithosphere”, Earth and Planetary Science Letters 105 (1991) 330-342.
[42] Lallemand S., Huchon P., Jolivet L., Prouteau G., Convergence lithosphe´rique Vuibert, Paris. Martin H., “Adakitic magmas: modern analogues of Archaean granitoids”, Lithos 46 (1999) 411–429.
[43] Wood D. A., “The applications of a Th–Hf–Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province”, Earth and Planetary Science Letters, 50 (1980) 11–30.
[44] Muller D., Groves D.I., “Potassic igneous rocks and associated gold-copper mineralization”, Springer., Berlin (1997) P 311.
[45] Pearce J. A., “Role of the sub-continental lithosphere in magma genesis at active continental margins. In: Continental Basalts and Mantle Xenoliths (Eds. Hawkesworth”, C. J. and Norry, M. J.) 230-249 (1983) Shiva, Nantwich, UK.
[46] Moayyed M., “New Attitude On Evolution of Neo-Tethys and its Relationship with Tertiary Magmatism in Urmia-Dokhtar and West Alborz -Azerbayjan (In persian)”, Proceedings of the 6th Conference of the Geological Society of Iran, Shahid Bahonar University, Kerman (2002) 374-378.
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