[1] Fenn P.M., “The nucleation and growth of alkali feldspars from hydrous melts”, Canadian Mineralogist 15 (1977) 135-161.
[2] London D., “Pegmatites”, Canadian Mineralogist Special Publication 10 (2008) 368.
[3] Rockhold J.R., Nabelek P.I., Glascock M.D., “Origin of rhythmic layering in the Calamity Peak satellite pluton of the Harney Peak Granite, South Dakota: the role of boron”, Geochimica et Cosmochimica Acta 51 (1987) 487–496.
[4] Kleck W.D., Foord E.E., “The chemistry, mineralogy, and petrology of the George Ashley Block pegmatite body”, American Mineralogist 84 (1999) 695–707.
[5] احمدی خلجی ا.، "پترولوژی توده گرانیتوئیدی بروجرد"، رساله دکتری، دانشکده علوم، دانشگاه تهران (1385).
[6] میرسپهوند ف.، طهماسبی ز.، شاهرخی س.، احمدی خلجی ا.، خلیلی م.، "ژئوشیمی و تعیین خاستگاه تورمالینهای منطقهی بروجرد"، مجله بلورشناسی و کانی شناسی ایران، شماره2 (1391) ص 281 – 292.
[7] Ahmadi Khalaji A., Esmaeily D., Valizadeh M.V., Rahimpour-Bonab H., “Petrology and geochemistry of the granitoid complex of Boroujerd, Sanandaj-Sirjan Zone, Western Iran”, Journal of Asian Earth Sciences 29 (2007) 859–877.
[8] Masoudi F., “Contact metamorphism and pegmatite development in the region S.W of Arak- Iran”, Thesis, University of Leeds. England. (1997) 321p.
[9] Masoudi F., Yardley B.W.D., Cliff R.A., “Rb-Sr geochronology of pegmatites, plutonic rocks and a hornfels in the south- west of Arak, Iran”, Journal of Sciences, Islamic Republic of Iran 13(3) (2002) 249-254.
[10] Afsharianzadeh A.M., Sahbaei M., “1/250000 map of Khorramabad, Geological Survey of Iran (in Persian)”, (1992).
[11] واعظیپور م.ج.، اقلیمی ب.، "یافتههای نوین در نهشتههای ژوراسیک ناحیه لکان (چهار گوش گلپایگان)"، گزارش داخلی، سازمان زمینشناسی و اکتشافات معدنی کشور(1363).
[12] Kertz R., ˝Symbol for rock- forming minerals˝, American Mineralogist 68(1983)277-9.
[13] London D., “The origin of primary textures in granitic pegmatites”, Canadian Mineralogist 47 (2009) 697–724.
[14] Pesquera A., Torres-Ruiz J., Gil-Grespo P. P., Velilla N., “Chemistry and genetic implications of tourmaline and Li-F-Cs micas from the Valdeflores area (Caceres, Spain)”, American Mineralogist 84 (1999) 55-69.
[15] Cameron E.N., Jahns R.H., McNair A.H., Page L.R., “Internal structure of granitic pegmatites”, Economic Geology Monograph 2 (1949) 115.
[16] Jahns R.H., “The study of pegmatites”, Economic Geology, 50th Anniversary (1955) 1025–1130.
[17] Jahns R.H., Tuttle O.F., “Layered pegmatite–aplite intrusive”, Mineralogical Society of America Special Paper 1 (1963) 78–92.
[18] Jahns R.H., “Internal evolution of pegmatite bodies”, Mineralogical Association of Canada Short Course Handbook, vol. 8 (1982) 293-327.
[19] Webber K.L., Falster A.U., Simmons W.B., Foord E.E., “The role of diffusion controlled oscillatory nucleation in the formation of line rock in pegmatite–aplite dikes”, Journal of Petrology 38 (1997) 1777–1791.
[20] London D., “A petrologic assessment of internal zonation in granitic pegmatites”, Lithos 184–187 (2014) 74–104.
[21] Van hinsberg V.J., Henry D.J., Marschall H.R., “Tourmaline an ideal indicator of its host environment”, The Canadian mineralogist, 49 (2011) 1-16.
[22] Slack J.F., Palmer M.R., Stevens B.P.J., Barnes R.G., “ Origin significance of tourmaline-rich rocks in the Broken Hill district, Australia”, Economic Geology 88 (1993) 505-541.
[23] Hawthorne F.C., Henry D.J., “Classification of the minerals of the tourmaline group”, European Journal of Mineralogy 11 )1999( 201-215.
[24] Trumbull R.B., Chaussidon M., “Chemical and boron isotopic composition of megmatic and hydrothermal tourmalines from the Sinceni granite-pegmaite system in Swaziland”, Chemical Geology 153 (1999) 125-137.
[25] London D., Manning D.A.C., “Chemical Variation and Significance of tourmaline from southwest England”, Economic Geology 90 (1995) 495-519.
[26] Pesquera A., Velasco F., “Mineralogy, geochemistry and geological significance of tourmaline-rich rocks from the Paleozoic Cinco Villas massif (western Pyrenees, Spain)”, Contributions to Mineralogy and Petrology 129 (1997) 53– 74.
[27] Pirajno F., Smithies R.H., “The FeO/ (FeO+MgO) ratio of tourmaline: A useful indicator of spatial variations in granite-related hydrothermal mineral deposits”, Journal of Geochemical Exploration 42 (1992) 371-381.
[28] Deer W.A., Howie A., Zussman J., “An introduction to the rock-forming minerals”, Long man, London (1991) 528p.
[29] Cavarretta G., Puxeddu M., “Schorl-Dravite- Ferridravite Tourmalines Deposited by Hedrothermal Magmatic Fluids during Early Evolution of the Larderico Geothermal Field”, Italy. Economic Geology 85 (1990) 1236-1251.
[30] Henry D.J., Guidotti Ch.V., “Tourmaline as petrogenetic indicator mineral: an example from staurolite-grade metapelites of NW Mains”, American Mineralogist 70 (1985) 1-15.