[1] Calagari A.A., “Fluid inclusion studies in quartz veinlets in the porphyry copper deposit at Sungun, East-Azarbaidjan, Iran” J. Asian Earth Sci. 23 (2) (2004) 179–189.
[2] Mikaeili K., Leybourne M., Sharifiyan S., “Evolution of the Magmatic-Hydrothermal System of the Anjerd Porphyry Cu(-Mo) Deposit, East-Azarbaijan, NW Iran”, Economic Geology 120 1 (2025) 119–135.
[3] Shokohi, H., Faridi, M., “Geological and Tectonic Map of the Sari-Nou Porphyry Body, Scale 1:1000, North of Marand” Project: Azarmeskan Iranian Company (2022). (In Persian).
[4] Whitney, D. L., Evans, B. W., “Abbreviations for names of rock-forming minerals” American mineralogist, 95(1) (2010) 185-187.
[5] Middlemost E. A. K., “A contribution to the nomenclature and classification of volcanic rocks” Geological Magazine 117 (1980) 51-57.
[6] Morrison G. W., “Characteristics and tectonic setting of the shoshonite rock association” Lithos13(1980) 97–108.
[7] Middlemost E.A.K., “Naming material in the magma igneous rock system” Earth – Science Reveiws 37 (1994) 215-224.
[8] Maniar P. D., Piccoli P. M., “Tectonic discrimination of granitoids” Geological society of America bulletin, 101(5) (1989) 635-643.
[9] Peccerillo A., Taylor S. R., “Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey” Contributions to mineralogy and petrology 58(1) (1976) 63-81.
[10] Harker A., “The natural history of igneous rocks” Methuen & Company (1909).
[11] Wilson M., “Igneous Petrogenesis” (1989) Springer.
[12] Rollinson H.R., “Using Geochemical Data: Evaluation, Presentation, Interpretation” (1993) Longman.
[13] Irvine T.N., Baragar W.R.A., “A guide to the chemical classification of the common volcanic rocks” Can. J. Earth Sci. 8 (5) (1971) 523–548.
[14] Winter J.D., “Principles of Igneous and Metamorphic Petrology” 2nd edn (2015) Pearson.
[15] Best M.G., “Igneous and Metamorphic Petrology” 2nd edn (2002) Wiley-Blackwell.
[16] Philpotts A.R., Ague J.J., “Principles of Igneous and Metamorphic Petrology” (2009) Cambridge Univ. Press.
[17] Villiger S., Ulmer P., Müntener O., “Equilibrium and fractional crystallization experiments at 0· 7 GPa; the effect of pressure on phase relations and liquid compositions of tholeiitic magmas” J. Petrol. 48 (1) (2007) 159–184.
[18] Bucholz C.E., Jagoutz O., Schmidt M.W., Sambuu O., “Fractional crystallization of high-K arc magmas: biotite-versus amphibole-dominated fractionation series in the Dariv Igneous Complex, Western Mongolia” Contrib. Mineral. Petrol. 168 (5) (2014) 1072.
[19] Boynton W.V., “Cosmochemistry of the rare earth elements: Meteorite studies” in: Henderson P. (Ed.), Rare Earth Element Geochemistry (1984) Elsevier, 63–114.
[20] Sun S.S., McDonough W.F., “Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes” in: Magmatism in the Ocean Basins, Geol. Soc. Lond. Spec. Publ. 42 (1989) 313–345.
[21] Zhou L., Ma C., She Z., “An Early Cretaceous garnet-bearing metaluminous A-type granite intrusion in the East Qinling Orogen, Central China: Petrological, mineralogical and geochemical constraints” Geosci. Front. 3 (5) (2012) 635–646.
[22] Srivastava R. K., Singh R. K., “Trace element geochemistry and genesis of Precambrian sub-alkaline mafic dikes from the central Indian craton: evidence for mantle metasomatism” Journal of Asian Earth Sciences 23(3) (2004) 373-389.
[23] Taylor S. R., McLennan S. M., “The geochemical evolution of the continental crust” Reviews of geophysics 33(2) (1995) 241-265.
[24] Gill J.B., “Mineralogy and Mineral Stabilities” in: Orogenic Andesites and Plate Tectonics (1981) Springer, 168–205.
[25] Galoyan G., Rolland Y., Sosson M., Corsini M., Melkonyan R., “Evidence for superposed MORB, oceanic plateau and volcanic arc series in the Lesser Caucasus (Stepanavan, Armenia)” C. R. Geosci. 339 (7) (2007) 482–492.
[26] Hoyle J., Elderfield H., Gledhill A., Greaves M., “The behaviour of the rare earth elements during mixing of river and sea waters” Geochim. Cosmochim. Acta 48 (1) (1984) 143–149.
[27] Henderson P., (Ed.) “Rare earth element geochemistry” Vol. 2 (2013) Elsevier.
[28] Humphris S.E., “The mobility of the rare earth elements in the crust” in: Developments in Geochemistry, Vol. 2 (1984) Elsevier, 317–342.
[29] Zheng Y. F., “Subduction zone geochemistry. Geoscience Frontiers” 10(4) (2019).1223–125.
[31] Pearce J. A., Peate D. W., “Tectonic implications of the composition of volcanic arc magmas” Annual Review of Earth and Planetary Sciences 23 (1995) 251–285.
[32] Pearce J. A., Stern R. J. “
Origin of back-arc basin magmas: Trace element and isotope perspectives”
Geophysical Monograph Series166 (2006) 63–86.
https://doi.org/10.1029/166GM06.
[33] Foley S.F., Tiepolo M., Vannucci R., “Growth of early continental crust controlled by melting of amphibolite in subduction zones” Nature 417 (2002) 837–840.
[34] Xu H., Zhang J., Wang Y., Liu W., “Late Triassic alkaline complex in the Sulu UHP terrane: Implications for post-collisional magmatism and subsequent fractional crystallization” Gondwana Res. 35 (2016) 390–410.
[35] Xiong X.L., Adam J., Green T.H., “Rutile stability and rutile/melt HFSE partitioning during partial melting of hydrous basalt: implications for TTG genesis” Chem. Geol. 218 (3-4) (2005) 339–359.
[36] Chen W., Zhang G., Ruan M., Wang S., Xiong X., “Genesis of intermediate and silicic arc magmas constrained by Nb/Ta fractionation” J. Geophys. Res. Solid Earth 126 (3) (2021) e2020JB020708.
[37] Gill J.B., “Orogenic andesites and plate tectonics” (2012) Springer.
[38] Brenan J.M., Shaw H.F., Ryerson F.J., Phinney D.L., “Mineral–aqueous fluid partitioning of trace elements at 900 °C and 2.0 GPa: constraints on the trace element chemistry of mantle melts” Geochim. Cosmochim. Acta 59 (16) (1995) 3331–3350.
[39] 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 (1992) 1–26.
[40] Pearce J.A., Harris N.B.W., Tindle A.G., “Trace element discrimination diagrams for the tectonic interpretation of granitic rocks” J. Petrol. 25 (4) (1984) 956–983.
[41] Barbarin B., “A review of the relationships between granitoid types, their origins and their geodynamic environments” Lithos, 46(3) (1999) 605-626.
[42] Sylvester P. J., “Post-collisional strongly peraluminous granites” lithos, 45(1-4) (1998) 29-44.
[43] Müller D., Groves D. I., “Tectonic settings of potassic igneous rocks”, In Potassic Igneous Rocks and Associated Gold-Copper Mineralization (1997) (pp. 11-38). Berlin, Heidelberg: Springer Berlin Heidelberg.
[44] Pearce J., “Sources and settings of granitic rock”, Episodes Journal of International Geoscience, 19(4) (1996) 120-125.
[45] Afshooni S.Z., Mirnejad H., Esmaeily D., Haroni H.A., “Mineral chemistry of hydrothermal biotite from the Kahang porphyry copper deposit (NE Isfahan), Central Province of Iran” Ore Geol. Rev. 54 (2013) 214–232.
[46] Taghavi S.A., Sadeghi M., Yazdi M., “Mineral chemistry of biotite and hornblende as indicators of magma evolution in granitoid plutons, Central Iran” Lithos 412-413 (2022) 106636.
[47] Nachit H., Ibhi A., Abia E.H., Ohoud M.B., “Discrimination between primary magmatic biotites, re-equilibrated biotites, and neoformed biotites” C. R. Geosci. 337 (16) (2005) 1415–1420.
[48] Tang P., Chen Y., Tang J., Wang Y., Zheng W., Leng Q., Wu C., “Advances in research of mineral chemistry of magmatic and hydrothermal biotites” Acta Geol. Sin. Engl. Ed. 93 (6) (2019) 1947–1966.
[49] Ashrafi N., Dabiri R., Jahangiri A., “Some chemical variations in biotite, phlogopite, and muscovite, considering their tectonic setting” Geopersia 14 (2) (2024) 307–325.
[50] Moshefi P., Hosseinzadeh M.R., Moayyed M., Lentz D.R., “Comparative study of mineral chemistry of four biotite types as geochemical indicators of mineralized and barren intrusions in the Sungun Porphyry Cu-Mo deposit, northwestern Iran” Ore Geol. Rev. 97 (2018) 1–20.
[51] Moshefi P., Hosseinzadeh M.R., Moayyed M., Lentz D.R., “Distinctive geochemical features of biotite types from the subeconomic Sonajil porphyry-type Cu deposit, northwestern Iran: Implications for analysis of porphyry copper deposit mineralization potential” J. Geochem. Explor. 214 (2020) 106543.
[52] Rieder M., Cavazzini G., Yakonov Y.D., Frank-Kanetskii V.A., Gottardi G., Guggenheim S., Koval P.W., Müller G., Neiva A.M.R., Radoslovich E.W., Robert J.L., Sassi F.P., Takeda H., Weiss Z., Wones D.R., “Nomenclature of the micas” Clays Clay Miner. 36 (3) (1998) 905–912.
[53] Foster M.D., “Interpretation of the composition of trioctahedral micas” U.S. Geol. Surv. Prof. Pap. 354 (B) (1960) 11–49.
[54] Abdel-Rahman A.M., “Nature of biotites from alkaline, calc-alkaline, and peraluminous magmas” J. Petrol. 35 (1994) 525–541.
[55] Munoz J.L., Swenson A., “Chloride-hydroxyl exchange in biotite and estimation of relation HCl/HF activities in hydrothermal fluids” Econ. Geol. 76 (1981) 2212–2221.
[56] Munoz J.L., “F–O–H, Cl–OH exchange in micas with applications to hydrothermal ore deposits” in: Micas, Rev. Mineral. 13 (1984) Mineral. Soc. Am., 469–493.
[57] Yang X.M., Lentz D.R., “Chemical composition of rock-forming minerals in gold related granitoid intrusions, southwestern New Brunswick, Canada: implications for crystallization conditions, volatile exsolution, and fluorine–chlorine activity” Contrib. Mineral. Petrol. 150 (2005) 287–305.
[58] Zhang C., Wang L.X., Koepke J., Wolff P.E., Wilke S., Almeev R.R., Stechern A., Holtz F., “A practical method for accurate measurement of trace level fluorine in Mg- and Fe-bearing mineral and glass using electron probe microanalysis” Geostand. Geoanal. Res. 40 (3) (2016) 351–363.
[59] Idrus A., “Petrography and mineral chemistry of magmatic and hydrothermal biotite in porphyry copper-gold deposits: a tool for understanding mineralizing fluid compositional changes during alteration processes” Indones. J. Geosci. 5 (2018) 47–64.
[60] Selby D., Nesbitt B.E., “Chemical composition of biotite from the Casino porphyry Cu–Au–Mo deposit, Yukon, Canada: Evaluation of magmatic and hydrothermal fluid chemistry” Econ. Geol. 95 (2) (2000) 183–196.
[61] Munoz J.L., Ludington S.D., “Flouride-hydroxyl exchange in biotite” Am. J. Sci. 274 (1974) 396–413.
[62] Parry W.T., Ballantyne J.M., Jacobs D.C., “Geochemistry of hydrothermal sericite from Roosevelt Hot Springs and the Tictic and Santa Rita porphyry copper systems” Econ. Geol. 79 (1984) 72–86.
[63] Chappell B.W., White A.J.R., “Two contrasting granite types: 25 years later” Aust. J. Earth Sci. 48 (4) (2001) 489–499.
[64] Bonin B., “Do coeval mafic and felsic magmas in post-collisional to within-plate regimes necessarily imply two contrasting sources?” Lithos 78 (1–2) (2004) 1–24.
[65] Whalen J.B., Currie K.L., Chappell B.W., Powell R., “A-type granites: Geochemical characteristics, discrimination and petrogenesis” Contrib. Mineral. Petrol. 95 (4) (1987) 407–419.
[66] Küster D., Harms U., “Post-collisional potassic granitoids from the southern and northwestern parts of the Late Neoproterozoic East African Orogen: a review” Lithos 45 (1-4) (1998) 177–195.
[67] Sun L., Wang Y., Fan W., Zi J., “Post-collisional potassic magmatism in the Southern Awulale Mountain, western Tianshan Orogen: petrogenetic and tectonic implications” Gondwana Res. 14 (3) (2008) 383–394.
[68] Abrecht J., Hewitt D.A., “Experimental evidence on the substitution of Ti in biotite” Am. Mineral. 73 (11-12) (1988) 1275–1284.
[69] Douce A.E.P., “Titanium substitution in biotite: an empirical model with applications to thermometry, O2 and H2O barometers, and consequence for biotite stability” Chem. Geol. 108 (1993) 132–162.
[70] Henry D.J., Guidotti C.V., Thomson J.A., “The Ti-saturation surface for low to medium pressure metapelitic biotite: Implications for geothermometry and Ti-substitution mechanisms” Am. Mineral. 90 (2005) 316–328.
[71] Helmy, H. M., Ahmed, A. F., El Mahallawi, M. M., Ali S. M., “Pressure, temperature and oxygen fugacity conditions of calc-alkaline granitoids, Eastern Desert of Egypt, and tectonic implications”, Journal of African Earth Sciences, 38(3) (2004) 255–268.
https://doi.org/10.1016/j.jafrearsci.2004.01.002
[72] Wones D.R., “Significance of the assemblage titanite+ magnetite+ quartz in granitic rocks” Am. Mineral. 74 (7-8) (1989) 744–749.
[73] Jacobs D.C., Parry W.T., “Geochemistry of biotite in the Santa Rita porphyry copper deposit, New Mexico” Econ. Geol. 74 (4) (1979) 860–887.
[74] Loferski, P.J., Ayuso, R.A., “Petrography and mineral chemistry of the composite Deboullie pluton, northern Maine, U.S.A.: implications for the genesis of Cu–Mo mineralization”, Chemical Geology, 123 (1995) 89–105.
[75] Boomeri M., Nakashima K., Lentz D.R., “The Sarcheshmeh porphyry copper deposit, Kerman, Iran: A mineralogical analysis of the igneous rocks and alteration zones including halogen element systematics related to Cu mineralization processes” Ore Geol. Rev. 38 (4) (2010) 367–381.
[76] Hassanpour S., Rahnama Z., Ebrahimi S., “Determination of physicochemical conditions of causative intrusion in the Masjeddaghi Cu-Au porphyry-epithermal deposit: constraints on chemical composition of biotite” Journal of Economic Geology 14, 4, (2022) 149–174.