[1] نظری غ.ح.، ترابی ق.، خلیلی م.، "بررسی شیمی کانیهای پریدوتیتهای گوشته افیولیت لوگر (جنوب غرب کابل- افغانستان)"، مجله علومزمین، شماره پنجم (بهار)1390 صفحه 19-48.
[2] Su B., Chen Y., Guo Sh., Liu J., "Origins of orogenic dunites: Petrology, geochemistry, and implications", International Association for Gondwana Research (2015) No of pages 19.
[3] Shafaii Moghadam H., Stern R. J., Chiaradia M., "Geochemistry and tectonic evolution of the Late Cretaceous Gogher- Bft ophiolite, central Iran", Lithos 168-169(2013) 33-47.
[4] Dilek Y., Delaloye M., "Structure of kizilda ophiolite, a slow – spread Cretaceous ridge segment north of the Arabian promontory", Geology 20(1992) 19-22.
[5] Hassanipak A. A., Ghazi A. M., "Petrology, geochemistry and tectonic setting of the Khoy ophiolite, Northwest Iran", Journal of Asian Earth science 18(1999) 43-55.
[6] Stocklin J., "Structural correlation of the Alpine range between Iran and Central Asia", Societe Geologie de la France Memoire Hors- Serve8 (1977) p 333-353.
[7] Abbate E., Bortolotti V., Principi G., "Apennine ophiolites: a peculiar oceanic crust", Ofioliti 1(1980) 59-96.
[8] عزیزیان ح.، نادری ن.، نوازی م.، پشت کوهی م.، رشیدی اچ.، "نقشه زمینشناسی 100000/1 برگه دولت آباد"، سازمان زمین شناسی ایران سری 346 (1385).
[9] Dick H. J. B., Bullen T., "Chromain spinel as a ptrogenetic indicator in abyssal and alpian – type peridotites and spacially associated lavas", Contrib Mineral Petrol 86(1984) 54-76.
[10] Maurel C., Maurel P., "Étude expérimentale de la distribution de láluminium entre bain silicate basique et spinelle chromifère. Implications pétrogénétiques: teneur en chrome des spinelles", Bulletin de Minéralogie 105(1982) 197-202.
[11] Kepezhinskas P. K., Defant M. J., Drummond M. S., "Na metasomatism in the island – arc mantle by slab melt – peridotite interaction: evidence from mantle xenoliths in the North Kamchatka arc", Journal of petrology 36(1995) 1505-1527.
[12] Sun S. S., McDonough W. F., "Chemical and isotopic systematic of oceanic basalts: implications for mantle composition and processes. In: Saunders, AD., Norry, M. J.(eds)Magmatism in the ocean Basin", Geological Seciety of London Special publication 42(1989) 313-345.
[13] Pearce J.A., Barker P.F., Edwards S.J., Parkinson I.J., Leat P.T., "Geochemistry and tectonic significance of peridotites from the South Sandwich arc-basin system, South Atlantic", Contribution to Mineralogy and Petrology 139(2000) 36-53.
[14] Suhr G., "Melt migration under oceanic ridges: Inferences from reactive transport modeling of upper mantle hosted dunites", Journal of Petrology 40(1999) 575-599.
[15] Koga K.T., Kelemen P.B., Shimizu N., "Petrogenesis of the Oman ophiolite", Geochemistry, Geophysics, Geosystems 2(2001) 2000GC000132.
[16] Bodinier J.L., Godard, M., "Orogenic, ophiolitic, and abyssal peridotites", In: Carlson, R.W. (Ed.) Treatise on Geochemistry vol 2 Elsevier (2003) pp 103–170.
[17] Piccardo G.B., Zanetti A., Müentener O., "Melt/peridotite interaction in the Southern Lanzo peridotite: field, textural and geochemical evidence", Lithos 94(2007) 181–209.
[18] Shahabpour J., "Tectonic evolution of the orogenic belt in the region located between Kerman and Neyriz", Jornal of Asian Earth Sciences 24 (2005) 405-417.
[19] Arai S., "Characterization of spinel peridotites by olivine-spinel compositional relationship: review and interpretation", Chemical Geology 113(1994) 191-204.
[20] Clos F., Gilio M., van Roermund H.L.M., "Fragments of deeper parts of the hanging wall mantle preserved as orogenic peridotites in the central belt of the Seve Nappe Complex, Sweden", Lithos 192–195(2014) 8–20.
[21] Xie Z.P., Hattori K., Wang J., "Origins of ultramafic rocks in the Sulu ultrahighpressure terrane, eastern China", Lithos 178 (2013) 158–170.
[22] Chen B., Suzuki K., Tian W., Jahn B.M., Ireland T., "Geochemistry and Os–Nd–Sr isotopes of the Gaositai Alaskan-type ultramafic complex fromthe northern North China craton: implications for mantle–crust interaction", Contributions to Mineralogy and Petrology 158(2009) 683–702.
[23] Ren Y.F., Yang J.S., Zhang Z.M., Li T.F., "Study of the Macaokuang peridotite body from the PP6 drill hole of the Chinese Continental Scientific Drilling (CCSD) project", Acta Geologica Sinica 81(2007) 1004–1016 (in Chinese with English abstract).
[24] Beyer E.E., Griffin W.L., O'Reilly S.Y., "Transformation of Archaean lithospheric mantle by refertilization: evidence from exposed peridotites in the Western Gneiss Region,Norway" Journal of Petrology 47(2006)1611–1636.
[25] Kubo K., "Dunite formation processes in highly depleted peridotite: case study of the Iwanaidake peridotite, Hokkaido, Japan", Journal of Petrology 43(2002) 423–448.
[26] Seo J., Oh C.W., Choi S.G., Rajesh V.J., "Two ultramafic rock types in the Hongseong area, South Korea: tectonic significance for northeast Asia", Lithos 175–176(2013) 30–39.
[27] Arai S., Ishimaru S., Mizukami T., "Methane and propanemicro-inclusions in olivine in titanoclinohumite-bearing dunites from the Sanbagawa high-P metamorphic belt, Japan: hydrocarbon activity in a subduction zone and Timobility", Earth and Planetary Science Letters 353–354(2012) 1–11.
[28] Zhang R.Y., Jahn B.M., Liou J.G., Yang J.S., Chiu H.Y., Chung S.L., Li T.F., Lo C.H., "Origin and tectonic implication of an UHPmetamorphicmafic–ultramafic complex from the Sulu UHP terrane, eastern China: evidence from petrological and geochemical studies of CCSD-Main Hole core samples", Chemical Geology 276(2010) 69–87.
[29] Song S.G., Su L., Niu Y.L., Lai Y., Zhang L.F., "CH4 inclusions in orogenic harzburgite: evidence for reduced slab fluids and implication for redox melting in mantle wedge", Geochimica et Cosmochimica Acta 73(2009b) 1737–1754.
[30] Song S.G., Su L., Niu Y.L., Zhang L.F., Zhang G.B., "Petrological and geochemical constraints on the origin of garnet peridotite in the North Qaidam ultrahigh-pressure metamorphic belt, northwestern China", Lithos 96(2007) 243–265.
[31] Oh C.W., Seo J., Choi S.G., Rajesh V.J., Lee J.H., "U–Pb SHRIMP zircon geochronology, petrogenesis, and tectonic setting of the Neoproterozoic Baekdong ultramafic rocks in the Hongseong Collision Belt, South Korea", Lithos 128–131(2012) 100–112.
[32] Mazzucchelli M., Rivalenti G., Brunelli D., Zanetti A., Boari E., "Formation of highly refractory dunite by focused percolation of pyroxenite-derived melt in the Balmuccia Peridotite Massif (Italy)", Journal of Petrology 50 (2009) 1205–1233.
[33] Ackerman L., Jelínek E., Medaris Jr., G., Ježek J., Siebel W., Strnad L., "Geochemistry of Fe-rich peridotites and associated pyroxenites from Horní Bory, Bohemian Massif: insights into subduction-related melt–rock reactions", Chemical Geology 259(2009)152–167.
[34] McDonough W.F., Sun S.S., "The composition of the Earth", Chemical Geology 120 (1995) 223–253.