[1] اتردی س. "کانی شناسی سیلیکات ها"، انتشارات دانشگاه پیام نور (1378) 291.
[2] Henry D.J., Guiditti C.V., “Tourmaline as a petrogenetic indicator mineral: an example from the staurolite grade metapelites of NW-Marine”, American Mineralogist, 70 (1985) 1-15.
[3] Harraz H. Z., El-Sharkawy M. F., “Origin of tourmaline in the metamorphosed Sikait pelitic belt, south eastern desert, Egypt”, Journal of African Earth Sciences, 33 (2001) 391-416.
[4] Deer W.A., Howie R.A., Zussman J., “Rock forming mineral”, Longman, (1) (1966) 333.
[5] London D., Manning D.A.C., “Chemical variation and significance of tourmaline from SW England”, Economic Geology, 90 (1995) 495–519.
[6] Novak M., Povandra P., Selway J.B., “Schorl–oxy–schorl to dravite–oxy–dravite tourmaline from granitic pegmatite, examples from the Moldanubicum, Czech Republic”, Europian Journal of Mineralogy, 16 (2004) 323-333.
[7] Bernard F., Moutou P., Pichavant M., “Phase relation of tourmaline leucogranites and the significance of tourmaline in silicic magma" Journal of Geology, 93 (1985) 271-291.
[8] Clemens J.D., Wall V.J., “Origin and crystallization of some peraluminous (S-type) ranitic Magmas”, Contribution to Mineralogy and Petrology, 19 (1981) 111-131.
[9] Brich W.D., Andrew J., Gleadow W., “The genesis of garnet and cordierite in acid volcanic rocks, Central Victoria, Australia”, Contribution to Mineralogy and Petrology, 45 (1974) 1-13.
[10] Thiele O., Alavi M., Assefi R., Hushmand–Zadeh A., Seyed–Emami K., Zahedi M., "Explanatory text of the Golpayegan quadrangle map. 1:250000”, Geological Survey Iran, (1968) 3-24.
[11] عبداللهی ش.، "مطالعهی پترولوژی توده نفوذی روستای ملاطالب (شمال الیگودرز) پهنه ی سنندج- سیرجان"، پایان نامه کارشناسی ارشد دانشگاه اصفهان (1388) 124.
[12] Chappell B.W., white A.J.R., “Two contrasting granite types”, Pacific Geology 8 (1974) 173-174.
[13] Kretz R., “Symbols for rock-forming minerals”, Americam Mineralogists 68 (1983) 277-279
[14] Hawthoren F.C., Henry D.J., “Classification of the mineral of the tourmaline group”, Europian Journal of Mineralogy, 11 (1999) 201-215.
[15] Hawthoren F.C., “Bond–valance constraints on the chemical composition of tourmaline”, Canadian Mineralogists, 40 (2002) 789-797.
[16] Collins A.C., “Mineralogy and geochemistry of tourmaline in contrasting hydrothermal system, Coplapo area, Northern Chile”, PhD Thesis, Faculty of Geoscience University of Arizona (2010).
[17] Einaudi M.T., Meinert L.D., Meinert R.J., “Newberry skarn deposit”, Economic Geology, 75th Anniversary special volume (1981) 317-391.
[18] Atherton M.P., “The variation in garnet, biotite, and chlorite composition in medium-grade pelitic rocks from the Dalradian, Scotland, with particular reference to the zonation in garnet”, Contribution to Mineralogy and Petrology, 18 (1968) 347-371.
[19] Taylor J., Setevens G., “Selective entrainment of peritectic garnet into S-Type granitic magmas: Evidance from Archean mid-crustal anatectites”, Lithos, 120 (2010) 277-292.
[20] Seprlich R., Giere R., Frey M., “Evolution of compositional polarity and zoning in tourmaline during prograde metamorphism of sedimentary rocks in the Swiss Central Alps.”, American Mineralogists, 81 (1996) 1222-1236.
[21] Henry D.J., Dutrow B.L., “Metamorphic tourmaline and its petrologic applications. In: Grew Es. Anovitz LM (eds) Boron. Mineralogy, Petrology and Geochemistry. The Mineralogical Society of America, Washington, Dc.”, Review Mineralogy 33 (1996) 503-557.
[22] Samson I.M., Sinclair W.D., “Magmatic hydrothermal fluids and the origin of quartz-tourmaline orbicules in the Seagull batholith, Yukon Territory”, Canadian Mineralogists, 30 (1992) 937-954.
[23] Truscott M.G., Shaw D.M., “Boron in chert and Precambrian siliceous iron formation”, Geochimca et Cosmochimca Acta, 48 (1984) 2220-2313.
[24] Torres–Ruiz J., Pesquera A., Gil–Crespo P.P., Velilla N., “Origin and petrogenetic implication of tourmaline–rich rocks in the Sierra Nevada (Betic Cordillera, Southeastern Spain)”, Chemical Geology, 197 (2003) 55-86.
[25] Wolf M.B., London D., “Boron in granitic magmas stability of tourmaline in equilibrium with biotite and cordierite”, Contribution to Mineralogy and Petrology, 130 (1997) 12-30.
[26] Gaweda A., Pieczka A., Kraczka J., “Tourmalines from the Western Tatra Mountains(W–Carpathians, S- Poland): Their characteristics and petrogenetic important”, Europian Journal of Mineralogy, 14 (2002) 943-955.
[27] طهماسبی ز، احمدی خلجی ا، رجاییه م، "تورمالینزایی در تودهی گرانیتوئیدی آستانه (جنوب غرب اراک)"، مجله بلورشناسی و کانی شناسی ایران، شماره 3 (1338) 369-380
[28] Yardley B.W.D., Rochelle C.A., Barnicoat A.C., Lioyd G.E., “Oscillatory zoning in metamorphic mineral: an indicator of infiltration metasomatism”, Mineralogical Magazine, 55 (1991) 357-365.
[29] Yuan C., Sun M., Xiao W., Wilde S., Li X., Liu X., Long X., Xia X., Ye K., Li J., “Garnet-bearing tonalitic porphyry from East Kunlun, Northeast Tibrtan Plateau: implications for adakite and magmas from the MASH Zone”, International Journal of Earth Sciences (Geol Rundsch), 98 (2009) 1489-1510.
[30] حسین میرزائی ز.، سپاهی ع.ا.، موذن م.، حسین میرزائی ز.، دادخواه ر.، "بررسی عوامل کنترل کنندهی ریخت شناسی بلورهای گارنت در سنگهای دگرگون و آذرین منطقه همدان"، مجله بلورشناسی و کانیشناسی ایران، شماره 4 (1389) 519-530.