]1[ آقانباتی ع.، "زمین شناسی ایران"، سازمان زمین شناسی و اکتشافات معدنی کشور،(1383)، ص 592
[2] Alavi M., "Sedimentary and structural characteristics of the Paleo-Tethys remnants in northeastern Iran", Geological Society of America Bulletin, 103(1991) 983-992.
]3[ رستمی حصوری م.، مظاهری ا.، "مطالعات پتروگرافی و ژئوشیمیایی سنگهای نفوذی کوهمیش سبزوار"، پایان نامه کارشناسی ارشد، دانشکده علومزمین، دانشگاه فردوسی مشهد، (1391)،168 صفحه
[4] صادقی ع.، "پترولوژی و ژئوشیمی توده گرانیتوئیدی ششتمد"، پایان نامه کارشناسی ارشد، دانشکده علومزمین، دانشگاه شاهرود، (1388)،230 صفحه.
[5] گوهرشاهی ر.، " پترولوژی، ژئوشیمی و تکتونیک توده گرانیتوئیدی مجاور کوه میش واقع در جنوب سبزوار"، پایان نامه کارشناسی ارشد(1380)
]6[ فارسی ز.، "پترولوژی و ژئوشیمی توده گرانیتوئیدی چاهسالار( جنوب غرب نیشابور)"، پایان نامه کارشناسی ارشد، دانشکده علومزمین، دانشگاه صنعتی شاهرود، (1388)
]7 [افتخارنژاد ج.، آقانباتی ع.، حمزهپور ب.، "نقشه 1:250000کاشمر"، سازمان زمینشناسی کشور،(1354)
]8[ جعفریان م.، جلالی ع.، " نقشه 100000/1 ششتمد"، سازمان زمینشناسی کشور.، (1377)
[10] Middle mostk.,”An introduction to Igneous petrology:Magmatic rocks”, Longmans Ed,(1985),pp. 266
[11] Irvine T.W.,Bargar W.R.A.,”Aguide to the chemical classification of the common volcanic rocks”,Canadian journal of Earth sciences,vol.8,(1971) ,pp.523-548.
[12] Harker A.," The natural history of igneous rocks", Methven, London (1909)
[13] Chappell B.W., White A.J.R., "I- and S-type granites in the Lachlan Fold Belt", Trans R Soc Edinburgh Earth Sciences. 83 (1992a) 1–26.
[14] Rickwood P. C, "Boundary lines within petrologic diagrams which use oxide of major and minor elements", LithosV. 22 (1989) 247-264.
[15] Maniar P. D, and Piccoli P. M., " Tectonic discrimination of granitoids", Geological society of America bulletinV. 101, (1984) 635-643
[16] Furnes H., El-Sayed M., Khalil S. O., "Pan African magmatism in the wadi –El-imradistrict, Central Desert, Egept: geochemistry& tectonic environment", Journal of, the Geological Society Vol. 153, (1996) 705-718
[17] Suns.s.,Mc Donough W.f.,”chemical and isotopic systematic of oceanic basalts:implications for processes.In:Magmatism in the ocean basins”,.Geol.soc.London specpulb.42,(1989).pp.313-345
[18] Mortimer N., Gans P.B., Mildenhall D. C., "A middle- late Quaternary age for the adakitic arc volcanic of Hautere (Solander Island), Southern Ocean", Journal of Volcanology and Geothermal Research. Vol 178, P701-707.
[19] Kovalenko V., Naumov V.B., Girnis A.V., Dorofeeva V.A and Yarmolyuk V.V.,"Average Composition of Basic Mantle Sourcces of Island Arcs and Active Continental Margins Estimated from the Data on Melt Inclusions and Quennched Glasses of rocks" ,Petrologhy. Vol 18, P1 -26.
[20] Sajona f.G., Maury R.C, Bellon H., Cotton j., Defant M.Hig “strength element of Pliocene-pleistocene island-arc basalt zamboanga peninsula western Mindanao.journal of petrology.37, (1996),pp.693-726.
[21] Wilson M., ”Ignous petrogenesis”.Unwin Hyman. (1989).
[22] Gill J. B., "Orogenic Andesites and plate Tectonics", Berling, springer verlay. (1981) 358pp.
[23] Hawkesworth C. J., Gallagher K., Hergt J. M., 1993, "Mantle and slab contributions in arc magmas", Annual Review of Earth and Planetary Science. Vol 21, P175-204.
[24] Keppler H., 1996, "Constraints from partitioning experiments on the composition of subduction zone fluids" ,Nature. Vol 380,P 237-240.
[25] Glenn A. G., 2004, "The influence of melt structure on trace element partitioning near the peridotite solidus". Contrib Mineral Petrol, 147, P 511-527.
[26] Kamber B. S., Ewart A., Collerson K. D., Bruce M. C., McDonald G. D. , 2002, "Fluid-mobile trace element constraints on the role of slab melting and implication for Archaean crustal growth models", Contrib Mineral Petrol, 144, P38-56.
[27] Chen B.Jahn B.M.,Ye K.,Liuj.B.” Cogenetic relationship of the Yangkou gabbro-to-granite unite,su-luterrane.j.geol.soc.london.(2002).159.
[28] Boynton W.V.," Geochemistry of the rare earth elements: meteorites studies. In: Henderson, P. (Ed.), Rare Earth ElementGeochemistry., Elsevier. 63 (1984)114
[29] Zhao Z.F., Zheng Y.F., Wei C.S., Wu Y.B.,"Post-collisional granitoids from the Dabie orogen in China: Zircon U-Pb age, element and O isotope evidence for recycling of subducted continental crust. Lithos. 93(2007) 248-272.
[30] Romick J.D., Kay S.M., Kay R.M.," The influence of amphibole fractionation on the evolution of calc-alkaline andesite and dasite tehpra from the central Aleutians, Alaska. Contrib. Mineral. Petrol.(1992) 112: 101-118.
[31] Hoskin P.W.O., Kinny P.D., Wyborn D., Chappell B.W," Identitifying accessory mineral saturation during differentiation in granitoid magmas: An integrated approach .J. Petrol. (2000) 41:1365-1395.
[32] Tepper J.H., Nelson B.K., Bergantz G.W., Irving A.J.," Petrology of the Chilliwack batholith, North Cascades, Washington:generation of calc-alkaline granitoids by melting of mafic lower crust with variable water fugacity",Contrib. Mineral.Petrol.(1993)113:333-351.
[33] Henderson P.,"Rare earth element geochemistry", Elsevier, Oxford, New York. (1984)
[34] Chappell B. W., White A. J. R.," Two contrasting granite types: 25years later, ustramin Journal of earth sciences", Vol, 48,.(2001) 489-499.
[35] Barbarin B.," Field evidence for successive mixing and mingling between the piolard diorite and the saintjulien-La-Vetre monzogranite(Nord-Fotez,Massif central,france)"can.j.Earth sci.,25, (1988) 49-59
[36] Didier J., Barbarin B.," Enclaves and granite petrology", Development in petrology .Elsevier, Amsterdam (1991)
[37] Boztug D., Ercin A. I., Kurucelik M. K., Goc D., Komur I., Iskendroglu A.,”Geochemical characteristics of the composite Kackar batholith generated in a Neo – Tethyan convergence system, eastern Pontides”, Turkey. Journal of Asian Earth Sciences, 27(2007),P 286 – 302.
[38] Bacon C.R., Druitt T.H.., "Compositional evolution of the zoned calcalkaline magma chamber of mount Mazama, Crater Lake, Oregon", Contributions to Mineralogy and Petrology 98(1998). P. 224-256.
[39] Bullen T. D., Clynne M. A., "Trace element and isotopic constraints on magmatic evolution at Lassen volcanic center", Journal of Geophysical Research 95(1995).P. 1967-1969.
[40] Rogers N. W., Hawkesworth C. J., Ormerod D. S., "Late Cenozoic basaltic magmatism in the Western Great Basin California and Nevada", J. Geophys. Res. 100(1995). P. 1028-1030.
[41] Weaver B. L., Tarney J., "Empirical approach to estimating the composition of the continental crust", Nature, 310(1984). P. 575-577.
[42] Wolf M. B., Wyllie J. P., ''Dehydration-melting of amphibolites at 10 kbar: the effects of temperature and time'', Contributions to mineralogy and petrology. 115, (1994), 369-383.
[43] Patino O., Douce A.E., "Effects of pressure and H2O content on the composition of melts primary crustal ", Trans. R.Soc. Edinburgh: Earth Science 87. (1996),pp:11-21.
[44] Patino O., Douce A.E., McCarthy T.C., "Melting of crustul rocks during continental collision and subduction, In: Geodynamics and geochemistry of ultrahigh-pressure rocks",Petrology and Structural Geology, Vol. 10. KluwerAcademic Publishers, Dordrecht. (1998),pp:27-55
[45] Altherr R., Holl A., Hegner E., Langer C., "High potassium,calc-alkaline, I-type plutonism in the EuropeanVariscides: northern Vosgos (France) northern Schwarzwald (Germany)", Lithos 50(2000), P. 51-37.
[46] Chappell B.W., White A.J.R., "Twocontrasting granite types", Pac. Geol., (1974)pp: 173-174
[47] Johannes W., Holtz F., "Petrogenesis andExperimental Petrology of Granitic Rocks", Berlin,Springer-Verlag(1996):P. 335.
[48] Pearce J., "Sources and setting granitic rocks", Episodes, 19 (4) (1996) 120-125.
[49] Harris N.B.W., Inger & R,XU."Cretaceous plutonism in central Tibet:an example of post collision magmatism?:" j.volcanol. Geotherm. res.,vol44,(1990) 21-32
[50] Pearce J.A., Harris B.W., Tindle A.G., “Trace element of iseriminant diagrams for the tectonic interpretation of granitic rocks”, Journal of petrology No 25(1984), PP.956-983
)