[1] Abdel-Rahman A.F.M., “Nature of biotites from alkaline, calc-alkaline, and peraluminous magmas”, Journal of Petrology (1994), 35(2), pp.525-541.
[2] Deer W.A., Howie R.A., Zussman J., “An Introduction to the Rock Forming Mineral”, Third
Longman Editions” (2013), 498 pp.
[3] Yavuz, F., “Evaluating micas in petrologic and metallogenic aspect: Part II—Applications using the computer program Mica+ Computers & geosciences”, (2003), 29(10), pp.1215-1228.
[4] Nash W.P., Crecraft H.R., “Partition coefficients for trace elements in silicic magmas”, Geochimica et Cosmochimica Acta (1985), 49(11), pp.2309-2322.
[5] Rasmussen K.L., Mortensen J.K., “Magmatic petrogenesis and the evolution of (F: Cl: OH) fluid composition in barren and tungsten skarn-associated plutons using apatite and biotite compositions: Case studies from the northern Canadian Cordillera”, Ore Geology Reviews (2013), 50, pp.118-142.
[6] Wones D.R., Eugster H.P., “Stability of biotite: Experiment, theory, and application”, American
Mineralogist (1965), 50: 1228-1272.
[7] Heinrich E.W., “Studies in the mica group; the biotite-phlogopite series”, American Journal of
Science (1946), 244(12): 836-848.
[8] Foster M. D., “Interpretation of the composition of trioctahedral micas”, Geol (1960). Surv. Prof. Paper. 354-B (1960) 49.
[9] Munoz J.L., “Calculation of HF and HCl fugacities from biotite compositions: revised equations”, Geological Society of America Abstracts with Programs (1992), 24: p. 221.
[10] López-Munguira1 A., Nieto F., Morata D., “Chlorite composition and geothermometry: a comparative HRTEM/AEMEMPA-XRD sltudy of Cambrian basic lavas from the Ossa Morena Zone”, SW Spain, Clay Minerals (2002) 37(2), 267-281. http://dx.doi. org/10.1180/0009855023720033.
[11] Nachit H., Ibhi A., Abia E.H., Ben Ohoud M., “Discrimination between primary magmatic biotites, reequilibrated biotites and neoformed biotites”, Comptes Rendus (2005). Géoscience 337, 1415–1420. https://doi. org/10.1016/j.crte.2005.09.002.
[12] Henry D., Guidotti C.V., Thomson J.,
“The Ti-saturation surface for low-to-medium pressure metapelitic biotites: Implications for geothermometry and Ti-substitution mechanisms”, American Mineralogist (2005) 90, 316– 328.
https://doi.org/10.2138/am.2005.1498.
[13] Li W., Cheng Y., Yang Z., “Geo‐fO2: Integrated software for analysis of magmatic oxygen fugacity Geochemistry”, Geophysics, Geosystems (2019), 20(5), 2542-2555.
[14] Cerny P., Burt D., “Paragenesis, crystallochemical characteristics, and geochemical evolution in micas in granite pegmatites”, In Micas (pp. 257-297). Reviews in Mineralogy (1984), Vol. 13, Min. Soc. America.
[15] Speer J.A., “Micas in igneous rocks”, Reviews in mineralogy (1984), 13(1), pp.299-356.
[16] Tischendorf G., Förster H.J., Gottesmann B., “Minor-and trace-element composition of trioctahedral micas: A review”, Mineralogical Magazine (2001), 65(2), pp.249-276.
[17] Barrière M., Cotton J., “Biotites and associated minerals as markers of magmatic fractionation and deuteric equilibration in granites”, Contributions to Mineralogy and Petrology (1979) 70:183–192.
[18] Van Lichtervelde M., Grégoire M., Linnen R.L., Béziat D., Salvi S., “Trace element geochemistry by laser ablation ICP-MS of micas associated with Ta mineralization in the Tanco pegmatite, Manitoba, Canada”, Contributions to Mineralogy and Petrology (2008), 155, pp.791-806.
[19] Neiva A.R., “Geochemistry of hybrid granitoid rocks and of their biotites from central northern Portugal and their petrogenesis”, Lithos (1981), 14(2), pp.149-163.
[20] Plá Cid J., Nardi L.V.S., Conceição H., Bonin B., “Anorogenic alkaline granites from northeastern Brazil: major, trace, and rare earth elements in magmatic and metamorphic biotite and Namafic minerals”, J Asian Earth Sci (2001) 19:375–397.
[21] Machev P., Klain L., Hecht L., “Mineralogy and chemistry of biotites from the Belogradchik pluton-some petrological implications for granitoid magmatism in Northwest Bulgaria”, In Annual Science Conference Geology (2004), pp. 16-17.
[22] Masoudi F., Jamshidi B.M., “Biotite and Hornblende composition used to investigate the nature and thermobarometry of Pichagchi pluton, northwest Sanandaj-Sirjan metamorphic belt, Iran” (2008).
[23] Karimpour M.H., Stern C.R., Mouradi M., “Chemical composition of biotite as a guide to petrogenesis of granitic rocks from Maherabad, Dehnow, Gheshlagh, Khajehmourad and Najmabad, Iran” (2011) 89-100.
[24] Beswick A. E., “An experimental study of alkali metal distributions in feldspars and micas”, Geochimica et Cosmochimica Acta (1973) 37:183–208.
[25] Wones D. R., “Contributions of crystallography, mineralogy, and petrology to the geology of the Lucerne pluton, Hancock County, Maine”, Am Mineral (1980) 65:411–437.
[26] Zhu C., Sverjensky D. A., “F–Cl–OH partitioning between biotite and apatite”, Geochimica et Cosmochimica Acta (1992) 56:3435–3467.
[27] Sallet R., “Fluorine as a tool in the petrogenesis of quartz-bearing magmatic associations: applications of an improved F-OH biotite–apatite thermometer grid”, Lithos (2000) 50:241–253.
[28] Ghorbani M., “Petrology and geochemistry of Mijan intrusive masses in the Jebal-e-Barez Mountains granitoid complex (southeast of Jiroft) (in persian)”, Earth Science Research, year 2, No.8, (2011), 19-35pp.
[29] Rahmanian Z., Ghadami Gh. A., Aahmadipour H., Poosti M., “Petrogenesis of granitoids from Dalfard area (Northwest of Jiroft): Evidence of Volcanic arc tectonic setting in Urumieh–Dokhtar magmatic belt”, Scientific Quarterly Journal, GEOSCIENCES, Vol. 33, Issue 1, Serial No. 127, Spring 2023, pp. 123-142.
[30] Behpour Sh., Moradian A., Ahmadipour H., “The origi, magma evolution and tectonic setting of southeast of Jebal-e-Baez granitoid, Bam, Kerman province (in persian)”, Scientific Quarterly Journal, GEOSCIENCE, Vol.29, No. 116, Summer 2020.
[31] Yazdanfar A., “Petrogenesis of delayed intrusive masses (Mijan, Hishin, Karur, Dara Hamzeh) in the Jabal Barez Batholith and its relationship with copper mineralization”, University of Shahid Beheshti, 2009. (in persian).
[32] Shafiei B., Haschke M., Shahabpour J., “Recycling of orogenic arc crust triggers porphyry Cu mineralization in Kerman Cenozoic arc rocks, southeastern Iran”, Mineralium Deposita (2009), 44, pp.265-283.
[33] Rasouli J., Ghorbani M., Ahadnejad V., Poli G., “Calk-alkaline magmatism of Jebal-e-Barez plutonic complex, SE Iran: implication for subduction-related magmatic arc”, Arabian Journal of Geosciences (2016), 9, 1-22.
[34] Hosseini M. R., Hassanzadeh J., Alirezaei S., Sun W., Li C. Y., “Age revision of the Neotethyan arc migration into the southeast Urumieh-Dokhtar belt of Iran: Geochemistry and U–Pb zircon geochronology”, Lithos (2017), 284, 296-309.
[35] Behpour S., Moradian A., Ahmadipour H., Nakashima K., “Mineralogy, petrology and geochemistry of mafic dikes in the southeast Jebal-E-Barez Granitoids (Bam, Kerman province, Iran): Studies from mafic dikes formed in avolcanic arc-setting”, Turkish Journal of Earth Sciences (2019), 28(6), 920-938.
[36] Nazarinia A., Mortazavi S.M., Arvin M., Poosti M., “Geothermobarometry of Sarmeshk granitoids in the Northwest of Sarduiyeh”, Petrological Journal (2018), 9(3), pp.173-192.
[37] Moghadam H.S., Griffin W.L., Santos J.F., Chen R.X., Karsli O., Lucci F., Sepidbar F., O'Reilly S.Y., “Geochronology, geochemistry and petrology of the Oligocene magmatism in SE segment of the UDMB, Iran”, Lithos (2022a) 416–417, 106644.
[38] Moghadam H.S., Li Q.L., Griffin W.L., Stern R.J., Santos J.F., Ducea M.N., Ottley C.J., Karsli O., Sepidbar F., O'Reilly S.Y., “Temporal changes in subduction- to collision-related magmatism in the Neotethyan orogen: The southeast Iran example”, Earth-Science Reviews (2022b) 226, 103930.
[39] Babazadeh S., Ghalamghash J., Raeisi D., Santosh M., Furman T., Choi S.H., D'Antonio M., Heilimo E., Cottle J.M., “Arc magmatism associated with continental convergence in the SE segment of the UDMA, Iran: Insights from zircon geochronology and Hf–Sr–Nd–Fe isotopes”, Lithos (2024b), 466, p.107468.
[40] Valeh N., “Geological Map of Iran Sheet 7647 Jebal Barez”, Geological Survey of Iran (1972), Tehran.
[41] Grabeljsek V., Cvetic S., Dimitrijevic M. N., “Geological Map of Iran Sheet 747-Sabzevaran”, Geological Survey and Mineral Exploration of Iran (1972), Tehran.
[42] Berberian M., King G.C.P., “Towards a paleogeography and tectonic evolution of Iran”, Canadian Journal of Earth Sciences (1981) 18, 210–265.
[43] Omrani J., Agard P., Whitechurch H., Benoit M., Prouteau G., Jolivet L., “Arcmagmatism and subduction history beneath the Zagros Mountains, Iran: A new report of adakites and geodynamic consequences”, Lithos (2008) 106, 380–398.
[44] Chiu H.Y., Chung S.L., Zarrinkoub M.H., et al., “Zircon U-Pb age constraints from Iran on the magmatic evolution related to Neotethyan subduction and Zagros orogeny”, Lithos (2013) 162-163, 70–87.
[45] Luhr J.F., Carmichael I.S., Varekamp J.C., “The 1982 eruptions of El Chichón Volcano, Chiapas, Mexico: Mineralogy and petrology of the anhydritebearing pumices”, Journal of Volcanology and Geothermal Researc (1984) 23(1- 2), 69-108.
[46] Uchida E., Endo S., Makino M., “Relationship between solidification depth of granitic rocks and formation of hydrothermal ore deposits”, Resource Geology (2007) 57(1): 47–56.
[47] Anderson J.L., “Status of thermobarometry in granitic batholiths”, Earth and Environmental Science Transactions of the Royal Society of Edinburgh (1997) 87, 125-138.
[48] Whitney D.L., Evans B.W., “Abbreviations for names of rock-forming minerals”, American Mineralogist (2010) 95, 185–187.
[49] Rieder M., Cavazzini G., D'Yakonov Y.S., Frank-Kamenetskii V.A., Gottardi G., Guggenheim S., Koval P.V., Müller G., Neiva A.M.R., Radoslovich E.W., Robert J.L., Sassi F.P., Takeda H., Weiss Z., “Nomenclature of the micas”, Canadian Mineralogist (1998), v. 36, p. 905-912.
[50] Deer W.A., Howie R.A., Sussman J., “An introduction to the rock forming minerals”,
Longman Ltd (1992). 528 p.
[51] Forster H.J., Tischendorf G., “Reconstruction of the volatile characteristics of granitoidic magmas and hydrothermal solutions on the basis of dark micas: the Hercynian Postkinematic granites and associated high-temperature mineralization of the Erzgebirge (G.D.R)”, Chemie der Erade (Geochemistry) (1989), 49, 7-20.
[52] Siahcheshm K., Calagari A.A., Abedini A., Lentz D.R., “Halogen signatures of biotites from the Maher-Abad porphyry copper deposit, Iran: Characterization of volatiles in syn- to post-magmatic hydrothermal fluids”, Int. Geol (2012). Rev. 54, 1368-1353.
[53] Nachit H., Razafimahefa N., Stussi J.M., Carron J.P., “Composition chimique des biotites et typologie magmatique des granitoids”, Comtes Rendus Hebdomadaires de l’ Academie des Sciences (1985) 301 (11) 813–818.
[54] Patiño Douce A.E., “Titanium substitution in biotite: an empirical model with applications to thermometry, O2 and H2O barometries, and consequences form biotite stability”, Chemical Geology (1993), 108(1–4): 133–162.
[55] Stussi J.M., Cuney M., “Nature of biotites from alkaline, calc-alkaline and per-aluminous magmas by Abdel-Fattah M. Abdel-Rahman: a comment”, J. Petrol (1996). 37,1025–1029.
[56] Fleet M.E., “Rock-Forming minerals. Volume 3A: Micas, seconded”, The Geological Society of London (2003), pp. 325–585.
[57] Zhou Z. X., “The origin of intrusive mass in Fengshandong, Hubei province”, Acta Petrologica Sinica 1986 2(2), 59-70.
[58] Nockolds S.R., “The relation between chemical composition and paragenesis in the biotite micas of igneous rocks”, American Journal of Science (1947) 245, 401– 420.
[59] Abuquerque C.A., “Geochemistry of biotites from granitic rocks, northern Portugal”, Geochimica et Cosmochimica Acta (1973) 37, 1779 1802.
[60] Samadi R., Torabi G., Kawabata H., Miller N.R., “Biotite as a petrogenetic discriminator: Chemical insights from igneous, meta-igneous and meta-sedimentary rocks in Iran”, Lithos (2021) 386–387, 106016. https://doi. org/10.1016/j.lithos.2021.106016.
[61] Shabani A.A.T., Lalonde A.E., Whalen J.B., “Composition of biotite from granitic rocks of the canadian appalachian orogen: a potential tectonomagmatic indicator?”, Canadian Mineralogist (2003) 41, 1381–1396.
[62] Jiang Y.H., Jiang S.Y., Ling H.F., Zhou X.R., Rui X.J., Yang W.Z., “Petrology and geochemistry of shoshonitic plutons from the western Kunlun orogenic belt, Xinjiang, northwestern China: Implications for granitoid geneses”, Lithos (2002) 63(3-4), 165-187.
[63] Anderson J.L., Barth A.P., Wooden J.L., Mazdab F., “Thermometers and thermobarometers in granitisystems”, Reviews in Mineralogy and Geochemistry (2008) 69, 121–142.
[64] Kilinc A., Carmichael I., Rivers M., Sack R., “The ferric-ferrous ratio of natural silicate liquids equilibrated in air”, Contributions to Mineralogy and Petrology (1983) 83: 136–140.
[65] Botcharnikov R., Koepke J., Holtz F., Mc Cammon C., Wlike M., “The effect of water activity on the oxidation and structural state of Fe in a ferro-basaltic melt”, Geochimica et Cosmochimica Acta (2005) 69: 5071– 5085.
[66] Moretti R., “Polymerisation, basicity, oxidation state and their role in ionic modeling of silicate melts”, Annales Geophysicae (2005) 56: 340–368.
[67] France L., Koepke J., Ildefonse B., Cichy S. B., Deschamps F., “Hydrous partial melting in the sheeted dike complex at fast-spreading ridges: Experimental and natural observations”, Contributions to Mineralogy and Petrology (2010) 160: 683–704.
[68] Ishihara S., “Major molybdenum deposits and related granitic rocks in Japan”, Rep. Geol. Surv. Japan (1971), 239, 1-178.
[69] Castro A., Stephen W. E., “Amphibole rich clots in calc-alkaline granitic rocks and their enclaves”, The Canadian Mineralogist (1992) 30: 1093–1112.
[70] Ishihara S., “The magnetite-series and ilmenite-series granitic rocks. Mining Geology, 27(145): 293-305.
[71] Wyborn D., Sun S. S., “Sulphur-undersaturated magmatism: A key factor for generating magma-related copper-gold deposits”. AGSO Research Newsletter (1977) 21: 7–8.
[72] Sun W. D., Arculus R. J., Kamenetsky V. S., Binns R. A., “Release of gold-bearing fluids in convergent margin magmas prompted by magnetite crystallization”, Nature (2004) 431: 975–978.
[73] Lalonde A. E, Bernard P., “Composition and color of biotite from granites; two useful properties in characterization of plutonic suites from the Hepburn internal zone of Wopmay Orogen, Northwest Territories”, Can Mineral (1993) 31:203–217.
[75] Tronnes R.G., Edgar A.D., Arima M., “A high pressure-high tempera-ture study of TiO2 solubility in Mg-rich phlogopite: Implications to phlogopite chemistry”, Geochimica et Cosmochimica Acta (1985), 49, 2323–2329.
[76] Arima M., Edgar A.D., “Substitution mechanisms and solubility of titanium in phlogopites from rocks of probable mantle origin”, Contributions to Mineralogy and Petrology (1981), 77, 288–295.
[77] Abrecht J., Hewitt D.A., “Experimental evidence on the substitution of Ti in biotite”, American Mineralogist (1988), 73, 1275–1284.
[78] Buddington A.F., Lindsley D.H., “Irontitanium oxide minerals and synthetic equivalent”, J. Petrology (1964) 5, 310-357.
[79] Kwak T.A.P., “Ti in biotite and muscovite as an indication of metamorphic grade in almandine amphibolite facies rocks from Sudbury, Ontario”, Geochimica et Cosmochimica Acta (1968) 32, 1222–1229. https://doi. org/10.1016/0016-7037(68)90124-5.
[80] Hibbard M.J., “Petrography to petrogenesis”, Prentice Hall (1995), 587.
[81] Cathelineau M., Nieva D., “A chlorite solid solution geothermometer The Los Azufres (Mexico) geothermal system”, Contribution to Mineralogy and Petrology (1985), 91: 235-244.
[82] Walshe J. L., “A six component chlorite solid solution model and the conditions of chlorite formation in hydrothermal and geothermal systems”, Economic Geology (1986), 81: 681-703.
[83] De Caritat P., Hutcheon I.A.N., Walshe J.L., “Chlorite geothermometry: a review”, Clays and Clay Minerals (1993) 41, 219-239.
[84] Vidal O., De Andrade V., Lewin E., Munoz M, Parra T., Pascarelli S., “P-T-deformation-Fe3+/Fe2+ mapping at the thin section scale and comparison with XANES mapping: application to a garnet-bearing metapelite from the Sambagawa metamorphic belt (Japan)”, Journal of Metamorphic Geology (2006), 24(7), 669– 683.
[85] Inoue A., Kurokawa K., Hatta T., “Application of chlorite geothermometry to hydrothermal alteration in Toyoha geothermal system, Southwestern Hokkaido”, Japan. Resource Geology (2010), 60, 52–70.
[86] Bourdelle F., Cathelineau M., “Low-temperature chlorite geothermometry: a graphical representation based on T-R2+-Si diagram”, European Journal of Mineralogy (2015) 27, 617-626.
)