[1] Camp V. E., and Griffis R.J., "Character, genesis and tectonic setting of igneous rocks in the Sistan syture zone, eastern Iran". Lithos 15(1982) 221-239.
[2] Whalen J.B., Currie K.L., Chappell B.W., "A-type granites: geochemical characteristics, discrimination and petrogenesis". Contributions to mineralogy and petrology 95(1987) 407-419
[3] Bonin B., "A-type granites and related rocks: Evolution of a concept, problems and prospects", Lithos 97(2007) 1–29.
[4] Pitcher W.S., "The nature and origin of granite", Chapman & Hall, (1997) 387p.
[5] Sawkins F.J. "Metal deposite in relation to plate tectonic", Springer-Verlag, Heidelberg, New York, Tokyo, (1984) 325p.
[6] Mitchell A.H.G., and Granson, M.S., 1981, "Mineral deposits and global tectonic settings". Academic press, (1981) 405 p.
[7] Ishihara S., "The granitoid series and mineralization", Economic Geology, 75th Annive. V, Japan, 27(1981) 458-484.
[8] علوی نائینی م.، لطفی م.، "نقشه زمین شناسی 1:100000 نهبندان"، سازمان زمین شناسی و اکتشافات معدنی کشور(1989).
[9] علوی نائینی، م.، ، "نقشه زمین شناسی 1:250000 زابل"، سازمان زمین شناسی و اکتشافات معدنی کشور (1990).
[10] مهران ن.آ.، صادقی بجد م. و جوانشیر گیو، م.، "پیجویی و اکتشاف گرانیتهای منطقه بی بی مریم و افضلآباد"، طرح پژوهشی، دانشگاه بیرجند (1379).
[11] محمدی س.س.، "پتروگرافی و پتروژنز سنگهای گرانیتوئیدی نوار افیولیتی شرق ایران (ناحیه بیرجند-نهبندان)"، رساله دکتری، دانشگاه شهید بهشتی تهران (1386) .
[12] محمدی س.س.؛ وثوقی عابدینی،م.؛ امامی، م.ه.؛ خطیب، م.م.، "پتروگرافی، ژئوشیمی، منشأ و جایگاه تکتونیکی توده گرانیتوئیدی بی بی مریم(افضلآباد-نهبندان)"، فصلنامه علوم زمین، سازمان زمین شناسی و اکتشافات مواد معدنی کشور، شماره63 ، (1386) .
[13] Berberian M., King G.C.P., "Towards a paleogeography and tectonic evolution of Iran". Canadian Journal of Earth Sciences 18(1981) 210–265.
[14] Tirrul R., Bell I.R., Griffis R.J., CampV.E., "The Sistan suture zone of eastern Iran". Geological Society of America Bulletin 94(1983) 134-150.
[15] Middlemost, E.A.K., "Magmas and magmatic rocks" Longman scientific and Technical, (1985) 266p.
[16] Rickwood P.C., "Boundary lines within petrologic diagrams which use oxides of major and minor elements". Lithos 22(1989) 247–263.
[17] Barbarin B., 1999, "A review of the relationships between granitoid types, their origins and their geodynamic environments". Lithos 46(1999) 605-626.
[18] Chappell B.W.," Aluminium saturation in I- and S- type granites and the characterization of fractionated haplogranites", Lithos 46(1999) 535-551.
[19] Juteau T., and Maury R., "Geologie de la croute oceanique, petrologie et dynamique endogenes", Masson, Paris, (1997) 367p.
[20] Sun S.S., and McDonough W.F., "Chemical and isotopic systematic of oceanic basalts: implications for mantle composition and processes", in: Saunders, A.D., and Norry, M.J., eds., Magmatic in ocean basins. Geol. Soc. London. Spec. Pub. 42, (1989) pp. 313-345.
[21] Boynton W.V., "Geochemistry of the rare earth elements: meteorite studies". In : Henderson P., ed., rare earth elements geochemistry, Elsevier, (1984) 63-114.
[22] Harangi S., and Lenkey L., "Genesis of the Neogene to Qaternary volcanism in the Carpathian – Parnonian region : Role of subduction , extension ,and mantle plume", in beccaluva , L ,a , Bianchini ,G.,and Wilson ,M., (eds), Cenozoic volcanism in the Mediterranean Area :Geological society of America Specical Paper 418(2007) 67-92.
[23] Tatsumi Y., and Kogiso T., "Trace element transport during dehydration processes in the subducted oceanic crust": 2. Origin of chemical and physical characteristics in arc magmatism”, Earth and Planetary Science Letters 148(1997) 207-221.
[24] Pearce J.A., Harris N.B.W., Tindle A.G., "Trace element discrimenation diagrams for the tectonic interpretation of granitic rocks", J. Petrol 25 (1984) 956-983.
[25] Pearce J.A., and Parkinson I.J., "Trace elemet models for mantle melting: application to volcanic arc petrogenesis", From Prichard, H.M., Alabaster, T., Harris, N.B.W., and Neary C. R., eds., Magmatic Processes and Plate Tectonics, Geological Society Specical Publication No. 76(1993) 373-407.
[26] Stalder R., Foley S.F., Brey, G.P., Horn, L., " Mineral-aqueous fluid partitioning of trace elements at 900- 1200 ºC and 3-5.7 Gpa: new experimental data for garnet, clinopyroxene, and rutile, an implication for mantle metasomatism", Gechim. Cosmochim. Acta 62(1998) 1781-1801.
[27] Ayers J.C., "Trace modeling for aqueous fluid – peridotite inter action in the wedge of subduction zonnes", Conti. Mineral. Petrol 132(1998) 390-404.
[28] Moyen J.F., "High Sr/Y and La/Yb ratios: The meaning of the adakitic signature", Lithos 112(2009)556–574.
[29] Ayers , J.C., Watston ,E.B., " Solubility of apatite, monazite, zircon and rutil in super critical fluids with implications for subduction zone geochemistry", phil .Trans .R.Soc .London A , 335(1991)341-356.
[30] Brenan, J.M., shaw, H.F., Reyerson, F.J., Phinney, D.L., "Mineral-aqueous fluid partitioning of trace elements at 900°С and 2 Gpa : Constraints on the rare element chemistry of mantle and deep crustal fluids" , Geochim . Cosmochim. Acta 59(1995) 3331-3350.
[31] 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.
[32] Keppler, H., "Constraints from partitioning experiments on the composition of subduction Zone fluid" , Nature 380(1996) 237-240.
[33] Agostini, S., Doglioni, C., Innocenti, F., Manetti, P., Tonarini, s., and Savascin, M. Y., "The transition from subduction-related to intraplate Neogene magmatiasm in the Western Anatolia and Aegean area", in Beccaluva, L., Bianchini, G., and Wilson, M., eds., Cenozoic Volcanism in the Mediterranean Area: Geological Society of America. Special Paper 418(2007) 1-15.
[34] Martin, H., Smithies, R.H., Rapp, R., Moyen, J.F., and Champion, D., "An overview of adakite, tonalite-trondhjemite-granodiorite(TTG), and sanikitoid: relationships and some implications fot crustal evolution", Lithos 79(2005) 1-24.
[35] Martin, H., "Adakitic magmas: modern analogues of Archean granitoids", Lithos 46(1999)411-429.
[36] Defant, M.J., Drummond, M.S., "Derivation of some modern arc magmas by melting of young subducted lithospher", Nature 347(1990) 662-665.
[37] Rollinson, H.R., Tarney, J., "Adakites- the key to understanding LILE Depletion in granulites" , Lithos79(2005) 61-81.
[38] Gonza´lez-Partidaa, E., Levressea, G. , Carrillo-Cha´veza, A., Cheilletzb, A., Gasquetb, D., Jones, D., "Paleocene adakite Au–Fe bearing rocks, Mezcala, Mexico: evidence from geochemical characteristics", Journal of Geochemical Exploration 80(2003) 25–40.
[39] Drummond,M.S., Defant,M.J., Kepzhinskas, P.K.S., "Petrogenesis of slab-derived trondhjemite-tonalite-dacite/adakite magmas". Trans.R. Soc. Edinb. Earth Sci. 87(1996)205–215.
[40]Hoskin, P.W.O., and Schaltegger, U., "The composition of Zircon and Igneous and Metamorphi Petrogenesis" , in: Hunchar,J.M, and Hoskin, P.W.O., eds., Zircon: Reviews in Mineralogy and Geochemistry .V 53(2003) 27-62.
[41]Parrish, R.R., and Noble, S.R., "Zircon U-Th-Pb Geochronology by Isotope Dilution-Thermal Ionization Mass Spectrometry(ID-TIMS)" , in: Hunchar, J.M., and Hoskin, P.W.O., eds., Zircon: Reviews in Mineralogy and Geochemistry .V 53(2003)183-213.
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