[1] Maniar P. D., Piccoli P. M., "Tectonic discrimination of granitoides", Geo. Soc. of Am. Bull., Vol.101, (1989), 635-643.
[2] Irvine T. N., Baragar W.R.A., "A guid to chemical classification of the common volcanic rocks". Can. Jour. Earth. Sci., vol. 8, (1971), pp. 523-548.
[3] Sun S., McDonough W.F., "Chemical & isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Sounders, A.D., & Norry M. J., (eds), magmatism in oceanic basines". Geol. Soc. London. Spec.Pub.42, (1989), pp.313-348
[4] Boynton W.V., "Geochemistry of the Earth element meteorite studies". In: Henderson P.(ed),
Rare Earth Element geochemistry. Elsevier, (1984), PP. 63-114.
[5] Chappell, B. W. & White, A. J. R., "I and S-type granites in the Lachlan fold belt", Transactions of the Royal society of Edinburgh sciences,83, (1992), 1-26
[6] Chappell, B. W. & White, .A. J. R,"Two contrasting granite types : 25 years later", Australian Journal of earth sciences, vol. 48, (2001), 489-499.
[7] Berberian, F., & Berberian, M.," Tectono-Plutonic episodes in Iran". Geodynamics Series.
Vol. 3, (1983), 565-592.
]8[ معین وزیری، ح.، ًچند نقطه عطف در تاریخچه تکتونوماگمایی ایرانً، فصلنامه علمی - پژوهشی علوم زمین، سازمان زمین شناسی و اکتشافات معدنی، شماره 49-50، (1382 )، 39-32.
[9] Pearce, J. A., Harris, N.B.W& . Tindle, A. G., "Trace element Discrimination diagrams for the tectonic interpretation of granitic rocks". Journal of petrology, Vol. 25, part4, (1984), pp.956-983.
[10] Flierdt, T. V., Hoernes, S., Jung, S., Masberg, P., Hoffer, E., Schaltegger, U., Friedrichsen, H., "lower crustal melting and the role of open- system processes in the genesis of syn- orogenic quartz diorite- granite-leucogranite associatins: constraints from Sr- Nd-O isotopes from the Bandombaai complex, Namibia". Lithos 67,) 2003), 205-226.
[11] Opio-Aketch, N., Tarney, J. & Hoshino, M., "Petrology and geochemistry of granites from Archean terrain north of lake Victoria, Western Kenya". Journal of African Earth Sciences 29, (1999), 283-300.
[12] Patino Douce, A. E., "what do experiments tell us about the relative contributions of crust and mantle to the origine of granitic magmas?.In: Castro, A., Fernandez ,C., vigneressese, J. L. (eds), understanding granites: Intergrating New and classical Techniques", Geological Society of London, special publication 168, (1999), pp. 55-75.
[13] Wolf, M. B. & London, D., "Incongruen tdissolution of REE- and Sr rich apatite in peraluminous granitic liquids: differential apatite, monazite, and xenotime solubilities during anatexis". Am. Mineral. 80, (1995), pp. 765-775.
[14] Green, T. H. & Adam, J., "Pressure effect on Ti- or P-rich accessory mineral saturation in evolved granitic melts with differing K2O/Na2O ratios". Lithos 61, (2002), pp.271-282.
[15] Green, T. H. & Pearson, N.J., " Ti- rich phase saturation in hydrous mafic– felsic compositions at high P,T." Chem. Geol. 54, (1986) 185-201.
[16] Ryerson F.J., Watson E.B., "Rutile saturation in magmas: implications for Ti- Nb- Ta depletion in island arc magma.". Earth Planet. Sci. Lett. 86, (1987), 225-239.
)