منشأ پلاژیوگرانیت‌ها و گابروهای افیولیت ملانژ بافت؛ واقع در جنوب غرب کرمان

[1] Kaur G., Mehta P.K., “The Gothara plagiogranite: evidence for oceanic magmatism in a non-ophiolitic association, North Khetri Copper Belt, Rajasthan, India?”,Journal of Asian Earth Sciences, 25 (2005) 805-819.

[2] شفائی مقدم ه.، “کمربند افیولیتی نائین-بافت: سن، ساختار و منشاء”، پایان نامه دکتری، دانشگاه شهید بهشتی تهران (1387).

[3] Arvin M., Robinson P.T., “The petrogenesis and tectonic setting of lavas from the Baft Ophiolitic Melange, Southwest of Kerman, Iran”, Canadian Journal of Earth Sciences, 31 (1994) 824-834.

[4] Srdic A., Dimitrijevic M.N., Cvetic S., Dimitrijevic M.D., “Geological map of Iran, Scale 1:100000 Series Sheet 7348-Baft”, Printed by: Offset Press Inc. Tehran.)1972.(

[5] Beard J.S., Day H.W., “Origin of gabbro pegmatite in the Smartville intrusive complex, northern Sierra Nevada, California”, American Mineralogist, 71 (1986) 1085-1099.

[6] Ahmadipour H., Rostamizadeh G., “Geochemical aspects of Na-metasomatism in Sargaz granitic intrusion (south of Kerman province, Iran)”, Journal of Sciences, Islamic Republic of Iran, 23 (2012) 45-58.

[7] Barker F., “Trondhjemite, definition, environment and hypotheses of origin”, In Barker, F. (ed.), Trondhjemites, dacites, and related rocks, (1979)1-12.

[8] Middlemost E.A.K., “Naming materials in the magma/igneous rock system”, Earth Science Reviews, 37 (1994) 215-224.

[9] Irvine T.N., Baragar W.R.A., “A guide to the chemical classification of the common volcanic rocks”, Canadian Journal of Earth Sciences, 8 (1971) 523-545.

[10] Rickwood P.C., “Boundary lines within petrologic diagrams which use oxides of major and minor elements”, Lithos, 22 (1989) 247-263.

[11] Chappell B.W., White A.J.R., “Two contrasting granite types”, Pacific Geology, 8 (1974) 173-174.

[12] Shand S.J., “Eruptive rocks: Their genesis, composition, classification and their relation to ore deposites”, 3rd edition. Jhon Wiley and sons, New York,(1947) 488 p.

[13] Maniar P.D., Piccoli P.M., “Tectonic discrimination of granitoid”,Geological Society of America Bulletin, 101 (1989) 635-643.

[14] Christiansen E.H., Keith J.D., “Trace element systematics in silicic magmas: A metallogeneic prospective”,In: D.A. Wyman (ed.), Trace element geochemistry of volcanic rocks: applications for massive sulfide exploration. Geological Association of Canada, (1996) 115-151.

[15] Batchelor R.A., Bowden P., “Petrogenetic interpretation of granitoid rock series using multicationic parameters”, Chemical Geology, 48 (1985) 43-55.

[16] Pearce J.A., Harris N.B.W., Tindle A.G., “Trace element discrimination diagrams for the tectonic interpretation of granitic rocks”, Journal of Petrology, 25 (1984) 956-983.

[17] Harris N.B.W., Pearce J.A., Tindla A.G., “Geochemical characteristics of collision-zone magmatism”, In: M.P. Coward, A.C. Reis (eds.) Collision tectonics, Geological Society Special Publication, 19(1989) 67-81.

[18] Quanren Y., Zongqi W., Shuwen L., Qiugen L., Hongyuan Z., Tao W., Dunyi L., Yuruo S., Ping J., Jianguo W., Dehui Z., Jian Z., “Opening of the Tethys in Southwest China and its significance to the breakup of East Gondwanaland in late Paleozoic: Evidence from Shrimp U-Pb Zircon analyses for the Garze ophiolite block”, Chinese Science Bullentin, 50 (2005) 256-264.

[19] Kocak K., Isik F., Arslan M., Zedef V., “Petrological and source region characteristics of ophiolitic hornblende gabbros from the Aksaray and kayseri regions, Central Anatolian Crystalline Complex, Turkey”, Journal of Asian Earth Sciences, 25 (2004) 883-891.

[20] Bonev N., Stampfli G., “Gabbro, plagiogranite and associated dykes in the supra-subduction zone Evros Ophiolites, NE Greece”, Geological Magazine, 146 (2009) 72–91.

[21] Pearce J.A., “The role of the sub-continental lithosphere in magma genesis at destructive plate margins”, In: C.J. Hawkesworth, M.J. Norry (eds.), Continental basalts and mantle Xeoliths, (1983) 230-249.

[22] Meschede M., “A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb, Zr, Y diagram”, Chemical Geology, 56 (1986) 207-218.

[23] Rollinson H.R., “New models for the genesis of plagiogranites in the Oman ophiolite”, Lithos, 112 (2009) 603-614.

[24] Floyd P.A., Yaliniz M.K., Goncuoglu M.C., “Geochemistry and petrogenesis of intrusive andextrusive ophiolitic plagiogranites, Central AnatolianCrystalline Complex, Turkey”, Lithos, 42 (1998) 225-241.

[25] Flagler P.A., Spray J.G., “Generation of plagiogranite by amphibolite anatexis in oceanic shear zones”, Geology, 19 (1991) 70-73.

[26] Sun S.S., Mc Donough W.F., “Chemical and isotopic systematic of oceanic basalts: implications for mantle composition and processes”, In: A.D. Saunders, M. Norry, (eds.), Magmatism in Ocean Basins. Geological Society of London Special Publication, 42(1989) 313-345.

[27] Rapp R.P., Watson E.B., Miller C.F., “Partial melting of amphibolite, eclogite and the origin of Archean trondjemites and tonalities”, Precambrian Res., 51 (1991) 1-25.

[28] Lopez-Escobar L., “Plutonic and volcanic rocks from Central Chile (33o-42oS): geochemical evidence regarding their petrogenesis”, Ph.D. thesis, Massachusetts Institute of Technology, (1974) 270 p.

[29] Gao J., Klemd R., Long L., Xiong X., Qian Q., “Adakitic signature formed by fractional crystallization: An interpretation for the Neo-Proterozoic meta-plagiogranites of the NE Jiangxi ophiolitic mélange belt, South China”, Lithos, 110 (2009) 277–293.

[30] Dilek Y., Thy P., “Age and petrogenesis of plagiogranite intrusions in the AnkaraMélange, Central Turkey”, Island Arc, 15 (2006) 44-57.

[31] Berndt J., Koepke J., Holtz F., “An experimental investigation of the influence of water and oxygenfugacity on differentiation of MORB at 200 MPa”, Journal of Petrology, 46 (2005) 135-167.