مراجع
[1] Clemens J. D., “S-type granitic magmas- petrogenetic issues, models and evidence, Earth-Science Reviews”, 61(1-2) , (2003) pp. 1-18.
[2] Olsen S.N., marsh B.D., Baumgartner L.P., “Modeling mid crustal migmatite terrains as feeder zone for granite plutons; the competing dynamics of melt transfer by bulk versus porous flow. Translation of royal society of Edinburgh; Earth sciences”, 95, (2004) 49-58 .
[3] Rene M., Matejka D., Nosek T., “Geochemical constrains on the origin of a distinct type of two – mica granites (Destna – Lasenice type) in Moldanubian batholith (Czech Republic)”. Acta Montana,Ser. A 130, (2003) 59 – 76 .
[4] Rene M., Holtz F., Luo C., Beermann Stelling J., “Biotite stability in peraluminous granitic melts: Compositional dependence and application to the generation of two – mica granites in the South Bohemian batholiths (Bohemian Massif", Czech Republic). Lithos, 102, (2008) 538 – 553.
[5] Vigneresse J.L., Clemens J.D., “Granitic magma emplacement neither diapirism nor neutral buoyancy.” In: Vendeville, Y., Mart, Y., Vigneresse, J.-L. (Eds.), From the Arctic to the Mediterranean: Salt, Shale and Igneous Diapirs In and Around Europe. Special Publication of the Geological Society of London, vol. 174. Geological Society Publishing House, Bristol, (2000) pp. 1– 19.
[6] Clemens J.D., Mawer C.K., “Granitic magma transport by fracture propagation.” Tectonophysics 204, (1992) 339-360
[7] Petford N., Kerr R.C., Lister J.R., “Dike transport of granitic magmas.Geology 21”, (1993) 843-845
[8] Scaillet B., Pecher A., Rochette P., Champenois M., “The Gangotri granite (Garhwal Himalaya): lacolithic emplacement in an extending collisional belt.” J.Geophys.Res.,[Soild Earth] 100, (1995) 585-607
[9] Clemens J.D., “Observation on the origins and ascent mechanisms of granitic magmas”, J.Geol .Soc.(Lond.) 155, (1998) 843-851.
[10] موید محسن، موذن محسن، کلاگری علی اصغر، حسین زاده قادر، "کانی شناسی و پترولوژی توده گرانیتوئیدی میشو(جنوب غرب مرند – آذربایجان شرقی) و اهمیت ژئودینامیکی آن"، سیزدهمین همایش انجمن بلورشناسی و کانی شناسی ایران. دانشگاه کرمان .(1384) ، ص 141-146
[11] Sial A.N., Toselli A.J., Saavedra J., Parada M.A., Ferreira V.P., “Emplacment,petrological and magmatic susceptibility characteristics of diverse magmatic epidote-bearing granitoid rocks in Brazil”, Argentina and Chile.Lithos46, (1999) 367-392.
[12] Alcides N. Sial, Paulo M. Vasconcelos, Valderez P. Ferreira, Ricardo R. Pessoa, Roberta G. Brasilino, João M. Morais Neto., “Geochronological and mineralogical constraints on depth of emplacement and ascencion rates of epidote-bearing magmas from northeastern Brazil”, Lithos 105, (2008) 225–238
[13] Kretz R., “Symbols for rock forming minerals”, Am. Mineral. 68, (1983) 277 – 279
[14] Shelly D., “Igneous and metamorphic rocks under the microscope”, Chapman and Hail, (1993).
[15] R.H. Vernon, S.R. Paterson, “How late are K-feldspar megacrysts in granites?”, Lithos 104, (2008) 327–336
[16] Vernon R.H., “Quartz and feldspar microstructures in metamorphic rocks”, Canadian Mineralogist 37, (1999) 513 – 524.
[17] Vernon R.H., “A Practical Guide to Rock Microstructure”, Cambridge University Press, (2004) Cambridge.
[18] Ashworth J. R., Mclellan E.L., “textures, in : Ashworth, J. D. (ed) migmatites, blackie and Son, Glasgow”, (1985) 180-203.
[19] Dugan T. W., “Textural reletions in melanosomes of selected specimens of migmatitic pelitic schists: implications for leucosome- generation processes”, Cont. Mm. Pet., 83, (1983) pp. 82-98.
[20] Xu Cheng., Huang Z., Qi, L. Fu, P. Liu, C., Li, E., Guan T., “Geochemistry of cretaceous granites from Mianning in the Panxi region,Sichuan Province southweast china:Implications for their generation”, Journal of Asian Earth Sciences 29, (2007) 737-750
[21]Kalsbeek F., Jepsen H.F., Jones A., “Geochemistry and petrogenesis of S-type granite in East Greenland Caledonides”, Lithos,57. (2001a) 91-10
[22] Harris N., Inger S., Massey J., “The role of fluids in the formation of high Himalayan leucogranite.In: Treloar”, P.J., Searle M.P. (Eds.) Himalayan Tectonics. Special Publication Geological society of London, vol.74, (1993) pp. 391-400.
[23] Kalsbeek F., Hans F., Jepsen Allen P., Nutman “From source migmatites to plutons: tracking the origin of ca. 435 Ma S-type granites in the East Greenland Caledonian orogen.” Lithos, Volume 57, Issue 1, (2001b), 1-21
[24] Pearce A., Harris N.B., Tindle A.G., “Trace element discrimination diagrams for the tectonic interpretation of granitic rocks.”,Journa.Petrol.25:
(1984) 956-983.
[25] Talor S.R., McLennan S.M., “The continental crust: its composition and evolution”. Blackwell, Oxford 1985.
[26] Sylvester P.J., “Post – collisional strongly peraluminous granites”, Lithos 45, (1998) 29 – 44
[27] Chappel B.W., White A.J.R., Wyborn D., “The importance of residual source material (restites) in granite petrogenesis”, Journal of Petrology 28, (1987) 1111–1125
[28] Schmidt M.W., Thompson A.B., “Epidote in calc-alkaline magmas: and experimental study of stability”, phase relationship, and the role of epidote in magmatic evolution.American Mineralogist 81, (1996) 424-474
[29] Brandon A.D., Creaser R.A., Chacko T., “Constrain on rates of granitic magma transport from epidote dissolution kinetic”, science 271, (1996) 1845-1848
[30] Weinberg R.F., Sial A.N., Pessoa R.R., “Magma flow within the Tavares pluton, NE Brazil: compositional and thermal convection” Geological Society of America Bulletin 113, (2001) 508–520.
[31] Ghent E.D., Nicholls J., Simony P.S., sevigny J.H., Stout M.Z., “Hornblende geobarometry of the Nelson Batholith,southeastern British Columbia:tectonic implications”, Can.J.Earth science.2, (1991) 1982-19
[32] Zhang Z., Shen K., Sun W.D., Liu Y.S., Lio J.G., Shi C., Wang J.L., “Fluid in deeply subducted continental crust : Petrology , mineral chemistry and fluid inclusion of UHP metamorphic veins from the Sulu orogen, eastern China”, Geochemica et Cosmochemica Acta, 72 , (2008) 3200 – 3228.
[33] Evans B W., Vance J.A., “Epidote phonocrysts in dacitic dikes”, Boulder country, Colorado. Contrib. Mineral. Petrol. 96, (1987) 178-18
[34] Watson E.B., Harrison T.M., “Zircon saturation revisited:temperature and composition effects in variety of crustal magma types”, Earth Planet.Sci.Lett.64: (1983) 295-304.
[35] Patino Douce A. E., Beard J. S., “Dehydration-melting of biotite gneiss and quartz amphibolites from 3 to 15 kbar”, J. Petrol. 36, (1995) 707-738.
[36] Patino Douce A. E., Johnston A. D., “Phase equilibria and melt productivity in the pelitic system: implications for the origin of peraluminous granitoids and aluminous granites”, Contrib. Mineral. Petrol, (1991) 107: 202-218.
[37] Clemens J.D., Vielzeuf D., “constraints on melting and magma production in the crust” .Earth Planet.Sci.Lett. 86, (1987) 287 – 306
[38] Clemens J.D., Watkins J.M., “The fluid regime of hightemperature metamorphism during granitoid magma genesis”, Contrib. Mineral. Petrol. 140, (2001) 600–606.
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