بررسی سنگ شناسی، کانی شناسی و سنگ زایی پریدوتیت های سوره دال در جنوب ماشکان-شمال غرب ایران

[1] Windley B.F., “The evolving continents”. Wiley, New York. (1984) 385pp.

[2] Şengör A.M.C., Yilmaz Y., “Tethyan evolution of Turkey: a plate tectonic approach”. Tectonophysics 75 (1981) 181-241.

[3] Mohajjel M., Fergusson C.L., Sahandi M. R. “Cretaceous-Tertiary convergence and continental collision, Sanandaj-Sirjan Zone, Western Iran”. Journal of Asian Earth Sciences 21 (2003) 397-412.

[4] Stöcklin J. “Structural correlation of the Alpine ranges between Iran and central Asia” Societe Geol. France, Mdm. h. sdr, 8 (1977) 333-353.

[5] Golonka J., “Plate tectonic evolution of the southern margin of Eurasia in the Mesozoic and Cenozoic” Tectonophysics, 381 (2004) 235-273.

[6] Gilg H.A., Boni M., Balassone G., Allen C.R., Banks D., Moore F., “Marble hosted sulfide ores in the Angouran Zn- (Pb-Ag) deposit, NW Iran: interaction of sedimentary brines with a metamorphic core complex” Mineralium Deposita 41 (2006) 1-16.

[7] افتخارنژاد ج.، "تفکیک بخش های مختلف ایران از نظر وضع ساختمانی در ارتباط با حوضه های رسوبی" نشریه انجمن نفت، 82 (1359) 28- 19.

[8] خدابنده ع. ا.، سلطانی غ.، آقانباتی ع.، انوری ا.، "نقشه زمین شناسی 100000/1 نقده" سازمان زمین شناسی و اکتشافات معدنی کشور (1383).

[9] Deer W.A., Howie R.A., Zussman J., “An Introduction to the Rock Forming Minerals”, Second ed. Longman Scientific and Technical (1992) 696.

[10] Morimoto N., Fabries J., Ferguson A.K., Ginzburg I.V., Ross M., Sefert F., A., Zussman J., Aoki K., Gottardi G., Nomenclature of pyroxenes. Mineralogical Magazine 52 (1988) 535-550.

[11] Dick H.J.B., Bullen T., “Chromian spinel as a petrogenetic indicator in abyssal and alpin-type peridotites and spatially associated lavas”, Contribution to Mineralogy and Petrology 86 (1984) 54-76.

[12] Arai S., “Characterization of spinel peridotites by olivine-spinel composition. Relationships: review and interpretation” Chemical Geology 113 (1994a) 191-204.

[13] Pearce J.A., Lippard S.J., Roberts S., “Characteristics and Tectonic Significance of Supra-Subduction Zone Ophiolites”, Special Publications, Geological Society, London 16 (1984) 77-89.

[14] Shervais J. W., “Birth, death, and resurrection: the life cycle of suprasubduction zone ophiolites”, Geochemistry, Geophysics, Geosystems 2 (2001) 2000GC000080.

[15] Proenza J.A., Zaccarini F., Lewis J.F., Longo F., Garvit G., “Chromian spinel composition and the platinum-groupminerals of the PGE-rich Lomapegvera chromitites, Lomacaribe peridotite, Dominican Republic” Canadian Mineralogist 45 ( 2007) 631-648.

[16] Jan M.Q., Windley B.F., “Chromian spinel-silicate chemistry in ultramafic rocks of the Jijal complex Northwestern Pakistan”, Journal of Petrology 37 (1990) 667-715.

[17] Conrad W.K., Kay R.W., “Ultramafic and mafic inclusions from Adak island: crystallization history, and implications for the nature of primary magmas and crustal evolution in the Aleutian arc”, Journal of Petrology 25 (1984) 88-125.

[18] 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”, Contributions to Mineralogy and Petrology 139 (2000) 36-53.

[19] Arai S., “Compositional variation of olivine-chromian spinel in Mg-rich magmas as a guide to their residual spinel peridotites”, Volcanology and Geothermal Research 59 (1994b) 279-293.

[20] Irvin T.N., “Chromian spinel as a petrogenetic indicator, part 2. Petrologic applications”. Canadian Journal of Earth Science 4 (1967) 71-103.

[21] Leblanc M., Nicolas A., “Les chromitites ophiolitiques”, Chron. Rech. Miniere 507 (1992) 3-25.

[22] Arai S., “Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry”, Mineralogical Magazine 56 (1992) 173-184.

[23] Monnie C., Girardeau J., Maury R., Cotton, J., “Back- arc basin origin for the East Sulawesi ophiolite (eastern Indonesia)”, Geology 23 (1995) 851-854.

[24] Choi S.H., Shervais J.W., Mukasa S.B., “Suprasubduction and abyssal mantle peridotites of the coast range ophiolite, California”, Contributions to Mineralogy and Petrology 156 (2008) 551-576.

[25] Bloomer S.H., Hawkins J.W., “Gabbroic and ultramafic rocks from the Mariana trench: an island arc ophiolite. In: Hayes, D.E. (Ed.), The Tectonics and Geologic Evolution of Southeast Asian Sea and Islands: Part II, AGU Geophysical Monograph”, American Geophysical :union: 23 (1983) 294-317.

[26] Ishii T., Robinson P.T., Maekwa H., Fisker R., “Petrological studies of diapiric serpentinite seamounts in the Izu-Ogasawara-Mariana forarc” (1992).

[27] Bloomer S.H., Fisher R.L., “Petrology and geochemistry of igneous rocks from the Tonga trench- a non- accreting plate boundary”, Journal of Geology 95 (1987) 469-495.

[28] Parkinson I.J., Pearce J.A., “Peridotites from the Izu- Bonin-Mariana forearc (ODPLeg 125): evidence for mantle melting and melt- mantle interaction in a supra- subduction zone setting”, Journal of Petrology 39 (1998) 1577-1618.

[29] Hirose K., Kawamoto, T., “Hydrous partial melting of lherzolite at 1 GPa; the effect of H2O on the genesis of basaltic magmas”, Earth and Planetary Sciences Letters 133 (1995) 463-473.

[30] Van der Laan S.R., Arculus R. J., Pearce J.A., Murton B.J., “Petrography, mineral chemistry, and phase relations of the basement boninite series of site 786, Izu-Bonin forearc. In: fryer, P., Pearce, J.A., Stokking, L.B., et al. (eds)” Proceedings of the Ocean Drilling Program Scientific Result, 12”. College Station, Tx: Ocean Drilling Program (1992) 171-201.

[31] Sobolev A.V., Danyushersky L.V., “Petrology and geochemistry of boninites from the north termination of the Tonga Trench: constraints on the generation conditions of primary high-Ca boninite magmas”, Journal of Petrology 35 (1994) 1183-1211.

[32] Stern R.J., Johnson P.R., Kröner A., Yibas B., “Neoproterozoic ophiolites of the Arabian-Nubian Shield. In: Kusky, T.M. (Ed.), Precambrian Ophiolites and Related Rocks. In: Developments in Precambrian” Geology 13 (2004)95-128.

[33] Pagé P., Bédard J.H., Schroetter J.M., Tremblay A., “Mantle Petrology and Mineralogy of the Thetford Minos Ophiolite Complex”, Lithos 100 (2008) 255-292.

[34] Allahyari Kh., Saccani E., Pourmoafi M., Beccaluva L., Masoudi, F., ,” Petrology of mantle peridotites and intrusive mafic rocks from the Kermanshah ophiolitic complex (Zagros belt, Iran): implications for the geodynamic evolution of the Neo-Tethyan oceanic branch between Arabia and Iran”. Ofioliti, 35 (2) (2010) 71-90.

[35] Shafai Moghadam H, Stern R.J., “Late Cretaceous forearc ophiolites of Iran. Island Arc”, 20 (2010) 1-4.