[1] Jackson E.D., “Primary textures and mineral associations in the ultramafic zone of the Stillwater Complex, Montana”, U.S. Geological Survey Professional Paper 358 (1961) 106 p.
[2] Jackson E.D., “Ultramafic cumulates in the Stillwater, Great Dyke, and Bushveld intrusions”, in Wyllie, P. J., ed., Ultramafic and related rocks, New York, John Wiley (1967) 20-38.
[3] Jackson E.D., “The origin of ultramafic rocks by cumulus processes”, Fortschritte Mineralogie, 48 (1971) 128-174.
[4] Page N.J, Shimek R., Huffman C.Jr., “Grain-size variations within an olivine cumulate, Stillwater Complex, Montana”, U.S. Geological Survey Professional Paper 800-C (1972) C29-C37.
[5] Raedeke L.D., “Petrogenesis of the Stillwater Complex”, Seattle, Wash., University of Washington, Ph.D. dissertation (1982) 212 p.
[6] Raedeke L.D., McCallum I.S., “Investigations in the Stillwater Complex: Part II. Petrology and petrogenesis of the Ultramafic series”, Journal of Petrology 25 (1984) 395-420.
[7] Helz R.T., “Phase relations of basalts in their melting range at PH2o = 5 kb as a function of oxygen fugacity, Pt. 1, Mafic phases”, Journal of Petrology 14 (1973) 249-302.
[8] Oxburgh E. R., “Petrological evidence for presence of amphibole in the upper mantle”, Geol. Mag. 101 (1964) 1-19.
[9] Taylor H.P. Jr., “The zoned ultramafic complexes of southeastern Alaska”, In: Wyllie P. J. (ed) Ultramafic and related rocks. Wiley, New York, (1967) 97-121.
[10] Snoke A.W., Quick J.E., Bowman H.R., “Bear Mountain igneous complex, Klamath Mountains, California: an ultrabasic to silicic calk-alkaline suite”, J Petrol 22 (1981) 501-552.
[11] Nixon G.T., Cabri L.J., Laflamme J.H.G., “Platinum-group-element mineralization in lode and placer deposits associated with the Tulameen Alaskan-type complex”, British Columbia. Can Mineral 28 (1990) 503-535.
[12] Kepezhinskas P. K., Taylor R.N., Tansaka H., “Geochemistry of plutonic spinels from the north Kamchatka Arc: comparisons with spinels from other tectonic settings”, Mineral Mag 57 (1993) 575-589.
[13] Tistl M., Burgath K.P., Hohndorf A., Kreuzer H., Munoz R., Salinas R., “Origin and emplacement of Tertiary ultramafic complexes in northwest Colombia: evidence from geochemistry and K-Ar, Sm-Nd and Rb-Sr isotopes”, Earth Planet Sci Lett 126 (1994) 41-59.
[14] Feshtater G.B., Montero P., Borodina N.S., Pushkarev E.V., Smirnov V.N., Bea F., “Uralian magmatism: an overview”, Tectonophysics 276 (1997) 87-102.
[15] Hafez A.M.A., Abdel Kader Z., Shalaby I.M., “Zoned mafic-ultramafic complex in Wadi Abu Hamamid, South Eastern Desert”, Ann Geol Surv Egypt XVII (1991) 53-65.
[16] Droop G. T. R., “A general equation for estimating Fe3+ concentrations in ferromagnesian silicates and oxides from microprobe analyses, using stoichiometric criteria”, Mineralogical Magazine 51 (1987) 431-450.
[17] Alavi M., “Sedimentary and structural characteristics of the Paleo-Tethys remnants in northeastern Iran”, Geological Society of America Bulletin, 103 (1991) 9183-9192.
]18[ سبزهئی، م.، "پدیدههای تفریق در ماگماهای اولترابازیک: برداشتهایی از گدازههای لایهای اولترامافیک - مافیک اولاکوژنهای پالئو زوئیک ایران زمین"، سیزدهمین گردهمایی علوم زمین، سازمان زمین شناسی کشور، (1373) ص 65 – 78.
]19[ آقانباتی ع.، "زمین شناسی ایران، سازمان زمین شناسی و اکتشافات معدنی کشور"، (1383) 609 صفحه.
]20[ قائمی ف.، "نقشه زمینشناسی 1:25000 مشهد 5"، سازمان زمینشناسی و اکتشافات معدنی کشور، (1386).
]21[ قائمی ف.، "نقشه زمین شناسی 1:25000 مشهد 6"، سازمان زمین شناسی و اکتشافات معدنی کشور، (1386).
[22] Belov A.A., Gatinsky Yu.G., Mossakovsky A.A., “A precis on pre-Alpian tectonic history of tethyan paleooceans”, Tectonophysics 127 (1986) 197-211.
[23] Stöcklin J., “Possible Ancient Continental Margin in Iran”, In: Burk C.A. & C.L. Drake (eds) The geology of continental margins. Springer, Berlin, (1974) 873-887.
[24] Eftekharnejad J., Behroozi A., “Geodynamic significance of recent discoveries of ophiolites and late paleozoic rocks in NE Iran (including Kopet Dagh)”, Abhandlungen der Geologischen Bundesanstalt, 38 (1991) 89-100.
[25] Majidi B., “Etude pérostructurale de la région de Mashad (Iran). Les problèmes des méamorphites, serpentinites et granitoides hercyniens”, Thèse de Docteur Ingenieur, Université Scientifique ed Médicale de Grenoble, (1978) 277 pp.
[26] Majidi B., “The ultrabasic lava flows of Mashhad, North East Iran”, Geological Magazine 118 (1981) 49-58.
[27] Ghazi M., Hassanipak A.A., Tucker P.J., Mobasher K., “Geochemistry and 40Ar- 39Ar ages of the Mashhad Ophiolite, NE Iran”, Eos. Trans. AGU 82, (47), Fall Meet ( 2001)
[28] Shafaii Moghadam H., Li X.H., Ling X.X., Stern R.J., Zaki Khedr M., Chiaradia M., Ghorbani G., Arai S., Tamura A., “Devonian to Permian evolution of the Paleo-Tethys Ocean: New evidence from U-Pb zircon dating and Sr-Nd-Pb isotopes of the Darrehanjir- Mashhad ophiolites”, NE Iran, Gondwana Research (2014), http://dx.doi.org/10.1016/j.gr.2014.06.009
[29] Zanchi A., Zanchetta S., Berra F., Mattei M., Garzanti E., Molyneux S., Nawab A., Sabouri J., “The Eo-Cimmirian (Late? Triassic) orogeny in north Iran”, Geological Society, London, Special Publications, 312 (2009) 31-55.
[30] Arai S., Fujii T., “Petrology of ultrabasic rocks from Site 395”, in Initial Reports of DSDP, 45 (1978) 587-594, Melson W.G., et al. (Eds.), Washington (US Govt. Printing Office).
[31] Juteau T., Berger E., Cannat M., “Serpentinized residual mantle peridotites from the MAR median valley, ODP Hole 670A (21o 10/ N, 45o 02/ W, Leg 109)”, Primary mineralogy and geothermometry, Proceedings of ODP Scientific Results, 106/109 (1990) 27-45.
[32] Whitney D.L., Evans B.W., "Abbreviations for names of rock-forming minerals", American Mineralogist. 95 (2010) 185-187.
[33] Leake B.E., Woolley A.R., Arps C.E.S., Birch W.D., Gilbert M.C., Grice J.D., Hawthorne F.C., Kato A., Kisch H.J., Krivovichev V.G., Linthout K., Laird J., Mandarino J.A., Maresch W.V., Nickel E.H., Rock N.M.S., Schumacher J.C., Smith D.C., Stephenson N.C.N., Ungaretti L., Whittaker E.J.W., Youzhi G., “Nomenclature of amphiboles: Report of the subcommittee on amphiboles of the International Mineralogical Association, Commission on new minerals and mineral names”, American Mineralogist 82 (1997) 1019-1037.
[34] Bazylev B.A., Silantiev S.A., Dick H.G.B. Konokova N.N., “Magmatic amphiboles and micas in oceanic peridotites and some specific features of the related magmas: 15o 20/ N MAR Fracture Zone”, Russian Journal Of Earth Sciences, 3 (2001) 219-234.
[35] Raudsepp M., Turnock A.C., Hawthorne F.C., “Amphibole synthesis at low pressure: what grows and what doesn't”, Eur. J. Mineral. 3 (1991) 983-1004.
[36] Raudsepp M., Turnock A.C., Hawthorne F.C., Sherriff B.L., Hartman J.S., “Characterization of synthetic pargasitic amphibole (Na Ca2 Mg4 M+3 Si6 Al2 O22 (OH,F)2 ; M+3 = Al, Cr, Ga, Sc, In) by infrared specffoscopy, Rietveld structure refinement, and 27Al, 29Si and 19F MAS NMR spectroscopy”, Am. Mineral. 72 (1987) 580-593.
[37] Welch M.D., Kolodziejski W., Klinowski J., “A multinuclear NMR study of synthetic pargasite”, Am. Mineral. 79 (1994) 261-268.
[38] Dawson J.B. and Smith J.V., “Upper-Mantle Amphiboles: A Review”, Mineralogical Magazine 45 (1982) 35-46.
[39] Cawthorn R.G., “The amphibole peridotite-metagabbro complex, Finero, northern Italy”, J. Geol. 83 (1975) 437-454.
[40] Coltori M., Siena F., “Mantle tectonite and fractionate peridotite at Finero (Italian Western Alps)”, Neues Jahrb. Mineral. Abh. 149 (1984) 225-244.
[41] Siena F., Coltori M., “The petrogenesis of a hydrated mafic-ultramafic complex and the role of amphibole fractionation at Finero (Italian Western Alps)”, Neues Jahrb. Mineral. Monatsh. (1989) 255-274.
[42] Arai S., Matsukage K., “Petrology of gabbro-troctolite-peridotite complex from Hess Deep, Equatorial pacific: implications for mantle-melt interaction within the oceanic lithosphere”, in: Proceedings of ODP, Scientific Results, 147 (1996) 135-148.
[43] Arai S., Matsukage K., Isobe E., Vysotskiy S., “Concentration of incompatible elements in oceanic mantle: effect of melt/wall interaction in stagnant or failed melt conduits within peridotite”, Geochim. Cosmochim. Acta, 61 (1997) 671-675.
[44] Frey F.A., Prinz, M., “Ultramafic inclusions from San Carlos, Arizona: petrologic and geochemical data bearing on their petrogenesis”, Earth Planet. Sci. Lett. 38 (1978) 129-176.
[45] Lensch G., “Die Ultramafitite der Zone von Ivrea und ihre geologische Interpretation”, Schweiz. Min. Pe!r. Mitt., 48 (1968) 91-102.
[46] Cannat M., Casey J.F., “An ultramafic lift at the Mid-Atlantic Ridge: successive stages of magmatism in serpentinized peridotites from the 15ºN region. In Vissers R.L.M., and Nicolas A. (Eds.), Mantle and Lower Crust Exposed in Oceanic Ridges and Ophiolites”, Dordrecht (Kluwer) (1995) 5-34.
[47] Silantyev S.A., “Origin conditions of the Mid-Atlantic Ridge plutonic complex at 13-17o N”, Petrology, 6 (1998) 351-387.
[48] Franz L., Becker K.P., Kramer W., Herzig P.M., “Metasomatic mantle xenoliths from the Bismarck microplate (Papua New Guinea): thermal evolution, geochemistry and extent of slab-induced metasomatism”, Journal of Petrology 43 (2002) 315–343.
[49] Coltorti M., Bonadiman C., Faccini B., Gregoire M., O'Reilly S.Y., Powell W., “Amphiboles from suprasubduction and intraplate lithospheric mantle”, Lithos 99 (2007) 68–84.
[50] Best M.G., “Mantle-derived amphibole within inclusions in alkalic-basaltic lavas”, J. Geophys. Res. 79 (1974) 2107–2113.
[51] Merrill R.B., Wyllie P.J., “Kaersutite and Kaersutite Eclogite from Kakanui, New Zealand Water-Excess and Water-Deficient Melting to 30 Kilobars”, Geological Society of America Bulletin, 86 (4) (1975) 555-570.
[52] Green D.H., Hibberson W.O., “The instability of plagioclase in peridotite at high pressure”, Lithos 3 (1970) 209–221.
[53] Ionov D., Griffin W.L., O'Reilly S.Y., “Volatile-bearing minerals and lithophile trace elements in the upper mantle”, Chemical Geology 141 (1997) 153–184.
[54] azylev B.A., Silantyev S.A., Kononkova N.N., “Phlogopite and hornblende in spinel harzburgites from the Mid-Atlantic Ridge: mineral assemblages and origin”, Ofioliti 24 (1999) 59–60.
[55] Ionov D.A., Hofmann A.W., “Nb–Ta-rich mantle amphiboles and micas: implications for subduction-related metasomatic trace element fractionations”, Earth and Planetary Science Letters 131 (1995) 341–356.
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