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Page 1: مجله بلورشناسی و کانی شناسی ایرانijcm.ir/article-1-378-fa.pdf · "+@ k," =kh k@ ! (-k4+g *h!"k n&-o,)p˚ˇ+@ q*kg˚:1 ( ˚+˚ ! -˚0 & ˚ 1 ) ... sample

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���� �S40��� !���� �S40��3"��$��:;%)���~ (~~�.[2] Deer W.A., Howie R.A., Zussman J., “Rock Forming Minerals, Double Chain Silicates”, 2nd Edition, London, Bath, Geological Society of London 2B (1997) 764 p. [3] Razavi M.H., Masoudi, F., Alaminia, Z., “Garnet-Biotite Chemistry for Thermometry of Staurolite Schist from South of Mashhad, NE Iran”, Journal of Sciences, Islamic Republic of Iran 19(3) (2008) 237-245. [4] Alavi M., Majidi B., “Petrology and geology of metamorphic and intrusive rocks of the Mashhad area”, Geological Survey of Iran (1972). [5] Alavi M., “Sedimentary and structural characteristics of the Paleo-Tethys remnants in northeastern Iran”, Geological Society of America Bulletin 103 (1991) 983-992. [6] Alavi M., “Thrust tectonics of the Binalood region, NE Iran”, Tectonics 11(2) (1992) 360-370. [7] Lammerer B., Langheinrch G., Danai M., “The tectonic evolution of Binaloud mountains. Geodynamic project (Geotraverse) in Iran”,Geological Survey of Iran 51 (1983) 519 P.

]�[=-O; �.��! � �%�).!.�%l�"�� �`.�&�?%!�@ � .�"����^40 �S40��3 ���� ! �S40��� � ��C4� ��*#"#� =�H *�

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[9] Majidi B., “Etude Petrostructurale de la ergion de Mashhad (Iran)”, These docteur, Ingeniever, University Science, de Grenoble, France (1978) 277 p.[10] Majidi B., “The geochemistry of ultrabasic and basic lava flows occurrences in northeastern Iran. In: Geodynamic Project in Iran”, Geological Survey of Iran report 51 (1983) 463-477. [11] Moazez Lesco Z., Plimer I.R., “Intrusive and Polymeta morphic Rocks of the Darakht-Bid Area, near Mashhad, Iran”, Band 68(1) (1978) 318-383. [12] Plimer I.R., Moazez Lesco Z., “Garnet Xenocrysts in the Mashhad Granite, NE Iran”, Geologische Rundschau 69(3) (1980) 801-810.

]��[�%l�"�� `.�"���%"# �%"#!"Z9 ! �O�5*wD �H!��&�O29 -�3� =�H"�$��9 �-5�% �0�45��@ ���� �23�%�

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[15] Karimpour M.H., Farmer L., Ashouri C., Saadat S., “Major, Trace and REE geochemistry of Paleo-Tethys Collision-Related Granitoids from Mashhad, Iran”, Journal of Sciences, Islamic Republic of Iran 17(2) (2006) 127-145. [16] Karimpour M.H., Stern C.R., Farmer L., “Zircon U-Pb geochronology, Sr-Nd isotope analyses, and petrogenetic study of the Dehnow diorite and Kuhsangi granodiorite (Paleo-Tethys), NE Iran”, Journal of Asian Earth Sciences 37 (2010) 384-393 [17] Alberti A., Nicoletti M., Petrucciani C., “K-Ar ages of micas of Mashhad granites (Khorasan, North-Eastern Iran)”, Period, Mineralogy 42 (1973) 483-493.[18] Homam S.M., “The occurrence and origin of atoll garnet in hornblende schists from the contact aureole of the Mashhad granite, NE iran”, Iranian Journal of Science and Technology 30 A1 (2006) 127-132. [19] Yuan C., Sun M., Xiao W., Wilde S., Li X., Liu X., Long X., Xia X., Ye K., Li J., “Garnet-bearing tonalitic porphyry from East Kunlun, Northeast Tibetan Plateau: implications for adakite and magmas from the MASH Zone”, International Journal of Earth Sciences (2008) DOI 10.1007/s00531-008-0335-y. [20] Leake B.E., Woolley A.R., Arps C.E.S., Birch W.D., Gilbert M.C., Grice J.D.F., Hawthorne C., Kato A., Kisch H.J., Krivovichev V.G., Linthout K., Laird J., Mandarino J., Maresch W.V., Nickel E.H., Rock N.M.S., Schumacher J.C., Smith D.C., Stephenson N.C.N., Ungaretti E.J.W., “Nomenclature of amphiboles, Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names”, European Journal of Mineralogy 9 (1997) 623-651. [21] Holland T., Blundy J., “Nonideal interactions in clacic amphiboles and their bearing on amphibole-plagioclase thermometry”, Contributions to Mineralogy and Petrology 116 (1994) 433-447. [22] Deer W.A., Howie R.A., Zussman J., “An Introduction to the Rock forming Minerals”, Longmans (1992) 696 p.

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]}�[� =-O;.�5�"�5 � �%� $.�"����# :M�H�:����@ ! �2Z0�] ��0�45���� �S40��3���"�-�3� )����(�

�(:;6��W�.[24] Harangi S.Z., Downes H., Ko´sa L., Szabo´ C.S., Thirlwall M.F., Mason P.R.D., “Almandine garnet in calc-alkaline volcanic rocks of the Northern Pannonian Basin (Eastern-Central Europe): geochemistry, petrogenesis and geodynamic implications”, Journal of Petrology 42 (2001) 1813-1843. [25] Samadi R., Mirnejad H., Shirdashtzadeh N., Kawabata H., “Petrology of tonalitic rocks of Dehnow (Northwest of Mashhad, Iran)”, Proceeding 1st International Applied Geological Congress (2010) 1265. [26] Kenah C., Hollister L.S., “Anatexis in the Central Gneiss Complex, British Columbia, in Migmatites, Melting and Metamorphism”, edited by Atherton M.P., Gribble C.D., Nantwich, England (1983) 142-162. [27] Schmidt M.V., “Amphibole composition in tonalite as a function of pressure: an experimental calibration of the Al in hornblende barometer”, Contributions to Mineralogy and Petrology 110 (1992) 304-310. [28] Green T.H., “Crystallization of calc-alkaline andesite under controlled high-pressure hydrous conditions”, Contributions to Mineralogy and Petrology 34 (1972) 150-166. [29] Green T.H., “Experimental phase equilibrium studies of garnet-bearing I-type volcanics and high-level intrusives from Northland, New Zealand”, Trans R Soc Edinb Earth Science 83 (1992) 429-438. [30] Green T.H., Ringwood A.E., “Origin of Garnet Phenocrysts in Calc-Alkaline Rocks”,Contributions to Mineralogy and Petrology 18 (1968) 163-174. [31] Skjerlie K.P., Johnston A.D., “Fluid-absent melting behavior of an F-rich tonalitic gneiss at mid-crustal pressures; implications for the generation of anorogenic granites”, Journal of Petrology 34 (1993) 785-815. [32] Vielzeuf D., Montel J.M., “Partial melting of metagreywackes, Part I. Fluid-absent experiments and phase relationships”, Contributions to Mineralogy and Petrology 117 (1994) 375-393.

[33] Patinao Douce A.E., Johnston A.D., “Phase equilibria and melt productivity in the pelitic system: implications for the origin of peraluminous granitoids and aluminous granulites”,Contributions to Mineralogy and Petrology 107 (1991) 202-218. [34] Green T.H., “Garnet in Silicic liquids and its possible use as a P–T indicator”, Contributions to Mineralogy and Petrology 65 (1977) 59-67. [35] Kawabata H., Takafuji N., “Origin of garnet crystals in calcalkaline volcanic rocks from the Setouchi volcanic belt, Japan”, Mineralogical Magazine 69 (2005) 951-971. [36] Kretz R., “Chemical study of garnet, biotite and hornblende from gneisses of Southwestern Quebec, with emphasis on the distribution of elements in co-existing minerals”, Journal of Geology 67 (1959) 371-402.[37] Green T.H., “Garnet in Silicic liquids and its possible use as a P-T indicator”, Contributions to Mineralogy and Petrology 65 (1977) 59-67. [38] Spear F.S., Cheney J.T., “A petrogenetic grid for pelitic schists in the system SiO2 - Al2O3 - FeO - MgO - K2O - H2O”, Contributions to Mineralogy and Petrology 101 (1989) 149-164. [39] Hensen D.J., Green D.H., “Experimental study of the stability of cordierite and garnet in pelitic compositions at high pressures and temperatures”, Contributions to Mineralogy and Petrology 38 (1973) 151-166. [40] Green T.H., Hellman P.L., “Fe-Mg partitioning between coexisting garnet and phengite at high pressure, and comments on a garnet-phengite geothermometer”, Lithos 15 (1982) 253-266. [41] Green T.H., “Experimental generation of cordierite or garnet-bearing granitic liquids from a pelitic composition”, Geology 4 (1976) 85-88. [42] Clemens J.D., Wall V.J., “Origin and crystallization of some peraluminous (S-type) granitic magmas”, The Canadian Mineralogist 19 (1981) 111-131. [43] Conrad W.K., Nicholls I.A., Wall V.J., “Water saturated and undersaturated melting of metaluminous and peraluminous crustal compositions at 10 kb: Evidence for the origin of silicic magmas in the Taupo Volcanic Zone, New Zealand,and other occurrences”, Journal of Petrology 29 (1988) 765-803.

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