]1 [افتخار نژاد ج.، وحدتی دانشمند ف.، " نقشه زمین شناسی چهار گوش بیرجند با مقیاس 1:250000، شماره ک "، سازمان زمین شناسی کشور. (1369).
]2 [افتخار نژاد ج.، "نقشه زمین شناسی بیرجند با مقیاس 1:100000"، سازمان زمین شناسی کشور. (1986).
]3[ زرینکوب م.ح.، "پترولوژی و ژئوشیمی مجموعههای افیولیتی جنوب بیرجند "، رساله دکتری. دانشگاه تربیت معلم تهران، تهران،(1379)، ص301.
]4 [یوسف زاده م.ح.، پورمعافی س.م.، سبزه ئی م.، وثوقی عابدینی م.، امامی م.ه.، "سنگشناسی و زمینشیمی آتشفشانی های دوران سوم در منطقهی بیرجند با تاکید بر انکلاوهای آن"، مجموعه مقالات چهاردهمین همایش انجمن بلورشناسی و کانیشناسی ایران، دانشگاه بیرجند، (1385)، ص 340- 348.
[5] Ohanian T., “The Birjand ophiolite an intercontinental transform structure eastern Iran”, Geological Survey of Iran . Report No. 51 ( 1983), pp. 239-245.
[6] Jung D., Keller J., Khorasani R., Marcks Chr., Baumann A., Horn P., "Petrology of the tertiary magmatit activity in the northern Lut area east of Iran”, Geological Survey of Iran . Report No. 51 (1983), pp. 239-245.
]7 [الله پور ا.، وثوقی عابدینی م.، امامی م.ه.، "ژئوشیمی و پترولوژی سنگ های آذرین خروجی ترشیری منطقه بیرجند "، مجله پژوهشی دانشگاه اصفهان (علوم پایه)،ج 20، شماره 2، (1383)، ص 121- 138.
[8] Tirrul R., Bell L. R., Griffis R.J., Camp V. E., “The sistan suture zone of eastern Iran”, G.S.A. Bulletin, Vol. 84(1983), pp. 134-150.
[9] Camp V.E., Griffis R.J., “Character, genesis and tectonic setting of igneous rocks in the Sistan syture zone, eastern Iran”, Lithos, Vol. 15(1982), pp. 221-239.
[10] Khatib M.M., Zarrinkoub M.H., “Morpho-tectonics and mechanism of emplacement of the andesitic ring in Givshad, east of Iran”, Geophysical Research Abstracts, Vol. 11 ( 2009), EGU2009-5359.
]11[ خطیب م.م.، زرینکوب م.ح.، "کنترلکنندههای ساختاری در دگرسانی سنگهای واقع در پهنه برشی بوشاد"، چهارمین همایش انجمن زمینشناسی ایران، دانشگاه تبریز( 1379) ص 375- 380.
[12] Middlemost E.A.K., “Magmas and magmatic rocks, An introduction to igneous petrology”, Longman ( 1988), 266 P.
[13] Middlemost E.A.K., “Naming materials in the magma/igneous rock system”, Earth Sci Rev 37 (1994), pp. 215-224.
[14] Hofman A.W., Jochum K.P., Seufert M., White W.M., “Nb and Pb in oceanic basalts: new constraintson mantle evolution”, Earth and Planetary Science Letters 79 (1986), pp. 33-45.
[15] Juteau T., Maury R., “Geologie de la croute oceanique, petrologie et dynamique endogenes”, Masson, Paris, (1997), 367p.
[16] Irvin J.N., Baragar W.K., “A guide to the chemical classification of the common volcanic rocks”, CAN. J. Earth. Sci. Vol. 8. (1971), pp. 523 – 548.
[17] Martin H., Smithies R.H., Rapp R., Moyen J.F., Champion D., “An overview of adakite, tonalite -trondhjemite-granodiorite(TTG), and sanikitoid: relationships and some implications fot crustal evolution “, Lithos, 79, (2005), PP. 1-24.
[18] Sun S.S., McDonough W.F., “Chemical and isotopic systematics 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.
[19] Rollinson H.R., “Using Geochemical Data: Evaluation, Presentation, Interpretation”, Longman ( 1993), 352 P.
[20] Tatsumi Y., 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), pp. 207-221.
[21] Harangi S., 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), pp. 67-92 .
[22] Pearce J.A., Harris N.B.W., Tindle A.G., “Trace elemet discrimenation diagrams for the tectonic interpretation of granitic rocks”, J. Petrol, 25 (1984), pp. 956-983.
[23] Pearce J.A., 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), pp. 373-407.
[24] 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), pp. 1781-1801.
[25] Ayers J.C., “Trace modeling for aqueous floid – peridotite inter action in the wedge of subduction zonnes”, Conti. Mineral. Petrol ,132(1998), 390-404.
[26] Best M.G., “Igneous and Metamorphic Petrology”, Second Edition, Blackwell Publishing, (2006), 729 p.
[27] Moyen J.F., “High Sr/Y and La/Yb ratios: The meaning of the adakitic signature" Lithos 112, (2009) , PP. 556–574.
[28] Ayers J.C., Watston E.B., “Solubility of apatite ,monazite ,zircon ,and rutite in super critical fluids with implications for subduction zone geochemistry ”, phil .Trans .R.Soc .LondonA ,335 ,(1991), PP. 341-356.
[29] Brenan J.M., shaw H.F., Reyerson F.J., Phinney D.L., “Mineral-aqueous fluid partitioning of trace elements at 900-1200°С and 3-5.7Gpa : new experimental data for garnet , clinopyroxne , and rotil , an implication for mantle metasomatism”, Geochim . Cosmochim. Acta, 62, (1998), PP. 1781-1801.
[30] 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), PP. 341-356.
[31] Keppler H., “Constraints from partitioning experiments on the composition of subduction Zone fluid”, Nature, 380,(1996), PP. 237-240.
[32] Agostini S., Doglioni C., Innocenti F., Manetti P., Tonarini s., 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), PP. 1-15.
[33] Tatsumi Y., Nakamura N., “Composition of aquaeous fluid from serpentinites in the subducted lithosphere”, Geochim. J. 20,(1986), PP. 191-196.
[34] Tatsumi Y., Hamilton D.L., Nesbitte R.W., “Chemical characteristics .of fluid phase from the subducted lithosphere: evidence from high-pressure experiments and natural rocks“, J. Volcanol. GeotHerm .Res. 29,(1986), PP.293-309 .
[35] Martin H., “Adakitic magmas: modern analogues of Archean granitoids“, Lithos, 46, (1999), PP. 411-429.
[36] Defant M.J., Drummond M.S., “Derivation of some modern arc magmas by melting of young subducted lithospher“, Nature, 347, (1990), PP. 662-665.
[37] Rollinson H.R., Tarney J., “Adakites- the key to understanding LILE Depletion in granulites“, Lithos, 79, (2005), PP. 61-81.
]38 [یوسف زاده م.ح.، پورمعافی س.م.، سبزه ئی م.، وثوقی عابدینی م.، امامی م.ه.، "سنگ شناسی و ژئوشیمی سنگهای آتشفشانی ترشیری شمال و غرب بیرجند و شناسایی برونبوم های آن "، مجله بلور شناسی و کانی شناسی ایران، سال هفدهم؛ شماره 2،(1388)، ص 213 – 230.
[39] Hoskin P.W.O., 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), PP. 27-62.
[40] Parrish R.R., Noble S.R., “Zircon U-Th-Pb Geochronology by Isotope Dilution-Thermal Ionization Mass Spectrometry(ID-hTIMS)“, in: Hunchar, J.M., and Hoskin, P.W.O., eds., Zircon: Reviews in Mineralogy and Geochemistry .V 53, (2003), PP. 183-213.