[1] Stocklin J., "Possible ancient continental margins in Iran. In: Burke C.A., Drake, C.L. (Eds.)", The Geology of Continental Margins Springer, New York, (1974) pp. 873–887.
[2] آقانباتی ع.، "زمینشناسی ایران"، انتشارات سازمان زمینشناسی و اکتشافات معدنی کشور. (1385) 586ص.
[3] Proenza J., Gervilla F., Melgarejo J.C., Bodinier J.L., “Al- and Cr rich chromitites from the Mayari-Baracoa Ophiolitic belt (eastern cuba)”, Consequence of interaction between volatile-rich melts and peridotites in suprasubduction mantle: Economic Geology, v.94, (1999) 547-566
[4] Boudier F., Nicolas A., “Harzborgite and lherzolite subtypes in ophiolitic and oceanic environments.”, Earth Planet. Sci. Lett. 76 (1985) 84-92.
[5] پژمان ل. ا.، "پیدایش کانسارها و منابع معدنی از دیدگاه مبانی ژئوشیمیایی" (1386).
[6] درویشزاده، ع. "سنگهای دگرگونی"، انتشارات پیام نور (1388).
[7] Irvin T.N., “Chromian Spinel as a Petrogenetic indicator”, part2. Petrologic applications: Canadian Journal of Eart Scifnces, v. 4, p.71-103. rocks. Can. J. Earth Sci., 8 (1967) 523-548.
[8] Coleman R. G., "Ophiolites", Springer Verlag, Berlin, (1977)229 p.
[9] Sabzehei M., “Rodingitization of Iranian basic rocks”, A new interpretation, Journal of Science, Islamic republic of Iran, 13( 2 ) ( 2002 ) 155-160.
[10] ترابی ق.، "بررسی رودنگیتیشدن دینامیکی و کانیشناسی آن در بخشی از مجموعهافیولیتی شمال انارک"، هشتمین همایش بلورشناسی و کانیشناسی ایران (1379).
[11] سبزه ای م.، "پترولوژی افیولیتهای ایران"، سازمان زمین شناسی کشور (1377).
[12] Schandle E.S., Hanley D.S.O, Wicks F.J., “Rodingites in serpentinized ultramafic rocks of the Abitibi greenstone belt, Ontario”,Canadian Mineralogist, (1989) 579-591
[13] وطنپور ح.، آفتابی ع.، "بررسی مهمترین انواع بافت و ساخت کانسارهای کرومیت در منطقه گفت و فرومد سبزوار"، فصلنامه علومزمین، شماره 23-24، سازمان زمینشناسی کشور (1376).
[14] ابراهیمی خ.، غلامی س.، "بررسی کانی شناسی- ژئوشیمیایی ذخایر کرومیت چاه یابوو چشمه پلنگی با نگرشی بر کاربرد صنعتی آنها"، مجله بلور و کانی شناسی ایران بهار 90، صفحه 167-182.
[15] ملک قاسمی ف.، کریم زاده ع. ر.، "بررسی کانه زایی پورفیری مس، مولیبدن و آهن در ناحیه قره چیلر - قره دره (شرق سیه رود - آذربایجان شرقی)"، ششمین همایش انجمن زمین شناسی ایران (1381).
[16] Yaghubpur A., Hassannejad A.A., “The Spatial Distribution of Some Chromite Deposits in Iran, Using Fry Analysis”, Journal of Sciences, Islamic Republic of Iran University of Tehran 17(2) (2006) 147-152.
[17] Leblanc M., Nicolas A., “Les Chromitites Ophiolitiques: Chronique de la Recherche Minier”, v.507 (1992) p.3-25.
[18] Nicolas A., “Structures of ophiolites and dynamic of oceanic lithosphere”, Kluwer, Dordrecht, (1989) 367 PP.
[19] Kamber B.S., Ewart A., Collerson K.D., Bruce M.C., McDonald G.D., "Fluid-mobile trace element constraints on the role of slab melting and implications for Archaean Crustal growth models", Contributions to Mineralogy and Petrology, v. 144 (2002) p. 38–56.
[20] Matveev s., Ballhaus C., “Role of water in the origin of podiform chromitite deposits”, Earth and Pelanetary Science Letters, v.203, (2002) p.235-243.
[21] Pearce J.A., Lippard S.J., Roberts S., "Characteristics and tectonic significance of supra-subduction zone Ophiolites. In: Kokelaar, B.P., Howells, M.F. (Eds.)", Marginal Basin Geology. Special Publication-Geological Society of London, vol. 6 (1984) pp. 77– 89.
[22] Rollinson H., ”Chromite in the mantle section of the Oman ophiolite: A new genetic model.”, The Island Arc, (2005) 542-550.
[23] Edwards S.J., Pearce J.A., Freeman J., "New insights concerning the influence of water during the formation of podiform chromite. In: Dilek, Y.,Moores, E.M., Elthon, D., Nicolas, A. (Eds.), Ophiolites and oceanic crust", new insights from field studies and the ocean drilling program. Geological Society of America Special Paper, vol. 349 (2000) pp. 139–147
[24] Arai S., “Chemistry of Chromian Spinel in volcanic rocks as a potential guide to magma chemistry”, Mineralogical Magazine, v.56 (1992) p.173-184
[25] Zhou M. F., Robinson P. T. Bai W, “Formation of Podiform Chromitites by melt/rock interaction in the upper Mantle”, V29 (1994) pp.98-101.
[26] Ferrario A., Garuti G., "Platinum-group minerals in chromite-rich horizons of the Niquelândia Complex (Central Goiás, Brazil)", Proc. Geo- Platinum Symp., Essex, U.K., (1988) pp. 261.272.
[27] Mussalam K., Junge D., Burgath K., "Textural features and chemical characteristic pf chromite in ultramafic rocks, Chalakidiki Complex(northeast Greece)", Tschermarks mineralogy, Petro. Mitt 29, (1981) 75-101.
[28] Dick H. J. B., Bullen T., "Chromian Spinel as a Petrogenetic indicator in abyssal and alpine type Peridotites and spatially associated lavas", Con. Min. Pet. 86 (1984) 54-76
[29] Kepezhinskas P. K., Taylor R. N., Tanaka H., "Geochemistry of plutonic Spinels from the north Kamchatka arc: comparisons with Spinels from other tectonic setting", Mineralogical Magazine, 57 (1993) 575-589.
[30] Virruete E.G., Estau’n A.P., Contreras F., Joubert M., Weis D., Ullrich T.D., Spadea P., “Plume mantle source heterogeneity through time: Insights from the Duarte Complex Hispaniola northastern Caribbean”, Journal of Geophysical Research 112 (2007) 1-19.
[31] Kerr A.C., Tarney J., Kempton P.D., Spadea P., Nivia A., SauMarriner G.F., Duncan R.A., “Pervasive mantle Plume head heterogeneity: Evidence from the lat Cretaceous Caribbean-Colombian oceanic plateau”, constraints” Jornal of Geophysical Research107 NO.B7.
[32] Kamenetsky V.S, Crawford A.J, Meffre S. "Factors controlling chemistry of magmatic Spinel: an empirical study of associated olivine", Cr-Spinel and melt inclusions from primitive rocks. J Petrol 42 (2001) 655–671.
[33] Sun S.S., McDonough W.F., "Chemicalandisotopic systematicsof oceanicbasalts: implications for mantle compositions and processes. In: Saunders A.D. and Norry M.J.(eds.)", Magmatism in ocean basins. Geol.Soc. London. Spec. Pub.42 (1989) pp. 313-345.
[34] Wilson M., "Igneous petrogenesis: a global tectonic approach", Unwin Hymen, London. (1989).
[35] Xia Q.-X. Zheng Y-F., Zhou L. G., "Dehydration and melting during continental collision: constraints from element and isotope geochemistry of low-T/UHP granitic gneiss in the Dabie orogen", Chem. Geol. 247 (2008) 36-65.
[36] Barnes S. J., Roeder P. L., "The range of spinel compositions in terrestrial mafic and ultramafic rocks", J. Pet., 42 (2001) 2279-2302
[37] Mikami M.H, “ Chromite in Industrial mineral and rocks by Lefond”, S J., American Institute of Mining, Metallurgica, and Petroleum Engineers, Inc by Prot City Press, Baltimor, Maryland (1983).
[38] Proenza J.A, Ortega Gutierrez F., Camprubi A., Tritlla J., Elias-Herrera M., Reyisalas M., “Paleozoic serpentinite-enclosed chromite from Tehrizingo (Acatlan complex Sothern Mecxico): a Petrological and mineralogical study”, J. of Sout American Earth Science 16 (2004) pp.547.
[39] امامعلی پور ع.، "بررسی کانی شناسی- ژئوشیمیایی کانی های فرعی و کمیاب همراه با نهشته های کرومیت خوی"، مجله بلورشناسی و کانی شناسی ایران زمستان 87، صفحه 559-570.