References
Arai, S., 1992-Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry, Mineral Mag., 56:173-184.
Arai, S. and Yurimoto, H., 1995-Possible Sub-arc origin of podiform chromitites, the Island arc, 4: 104-111.
Beccaluva, L., Di Girolamo, P., Macciotta, G. and Morra, V., 1983- Magma affinities and fractionation trands in ophiolites, Ofioliti, 8: 307-324.
Dike, H. J. B. and Bullen, T., 1984- Chromian spinel as a petrogenetic indicator in abyssal and alpine - type pridotites and spatially associated lavas, contrib. Mineral. Petrol., 86: 54-76.
Elipoulos, M. E. and Vacondis, I., 1995- Geochemistry of chromitites & host rocks from the Pindos ophiolite complex, northwestern Greece, Chemical Geology, 122: 99-108.
Ferrario, A. and Garuti, G., 1988- Platinum-group mineral inclutions in chromitites of the mafic-ultramafic complex (Ivrea-Zone,Italy). Mineral Petrol 41:125-143.
Jackson, E. D., 1969- Chemical variation in coexisting chromite and olivine in chromitite zones of the Stillwater complex: Economic Geol., Mon., 4:61-75.
Jackson, E. D. and Thayer, T. P., 1972- Some criteria for distinguishing between stratiform, concentric and alpine peridotite – gabbro complexes: Internat. Geol. Cong., 24th, Montreal, 1972, 2: 297-302.
Hassanipak, A. A. and Mohamad Ghazi, A., 2000- Petrolgy, Geochemistry and tectonic setting of the Khoy ophiolite, northwest Iran: implications for Tethyan tectonics, journal of Asian earth sciences, 18: 109-121.
Irvine, T. N., 1977- Origin of chromite layers in Maskox intrution and other stratiform intrutions: A new interpretation, geology, 5: 273-277.
Khalatbari-Jafari, M., Juteau, T., Bellon, H., Emami, H., 2003- Discovery of two ophiolite complexes of different ages in the Khoy area (NW Iran), CR Geosciences, Academie des Science, Paris, 335: 917-929.
Khalatbari-Jafari, M., Juteau, T., Bellon, H., Whitechurch, H., Cotton, J., Emami, H., 2004- New geological, geochronological and geochemical investigations on the Khoy ophiolites and related formations, NW Iran, J. Asian Earth Sci., 23: 507-535.
Khalatbari-Jafari, M., Juteau, T., Cotton, J., Emami, H., 2006- Petrological and geochemical study of the late Cretaceous ophiolite Khoy (NW Iran), and related geological formations, J. Asian Earth Sci., 27: 465-502.
Kamenetsky, V. S., Crawford, A. J., Meffre, S., 2001- Factors controling chemistry of magmatic spinel: an empirical study of associated olivine, Cr-spinel and melt inclutions from primitive rocks. Journal of Petrology, 42:655-671.
Leblanc, M. and Violette , J . F., 1983- Distribution of aluminum - rich and chromium - rich chromite pode in ophiolite peridotites, Econ. Geol., 78: 293-301.
Matveev, S. and Ballhaus, C., 2002- Role of water in origin of podiform chromitite deposits. Earth and Planetary Scince Letters, 203: 235-234.
Melcher, F., Grum, W., Simon, G., Thalhammer, T. V., Stumfl, F., 1997- Petrogenesis of the ophiolitic giant chromite deposits of Kempirisai, Kazakhstan: a study of solid and fluid inclusions in chromite, J. Petrol, 38: 1419-1458.
Menzies, M. A. and Allen, C., 1974- Plagioclase lherzolite residual mantle relationships within two eastern Mediterranean ophiolite. Contr. Mineralogy Petrology, 45: 197-213.
Pearce, J. A., Lippard, S. J. and Roberts, S., 1984- Characteristics and tectonic significance of supra -subduction ophiolites, In: B. P. Kokelaar and M. F. Howells (Eds.), Marginal basin geology, Geol. soc., London, spec. pub., pp. 777-794.
Proenza, J. A., Gervilla, F., Melgarejo, J. C., Bondinier, J. L., 1999- Al and Cr rich chromitites from the Mayari-Baracona ophiolitic belt (eastern Cuba): consequence of interaction between volatile-rich melts and peridotite in suprasubduction mantle, Econ. Geol., 94:547-566.
Roberts, S., 1988- Ophiolitic chromitite formation: a marginal basin phenomenon? Econ. Geol., 83: 1034-1036.
Rocci, G., Baroz, F., Bebien, J., Desmet, A., Lapierre, H., ohnenstetter, D. and Parrot, J. F., 1980- The Mediterrananean ophiolites and their related Mesozoic volcano- sedimentary sequences, in Panayiotou, A., ed., Proceedings of international ophiolite symposium, 1979, Cyprus, p. 273-286.
Thayer, T. P., 1964- Principal features and origin of podiform chromite deposites and some observations on the Guleman, Turkey, Econ. Geol., 59: 1497-1524.
Uysal, I., Sadiklar, M. B., Tarkian, M., Karsli, O. and Aydin, F., 2005- Mineralogy and composition of the chromitites and their platinum-group minerals from Ortaca (SW Turkey): evidence for ophiolitic genesis, Mineralogy and petrology, 83: 219-242.
Zaccarini, F., Pushkarev, E., Garuti, G., 2001- Plutinum-group element mineralogy and geochemistry of chromitite of the Kluchevskoy ophiolite complex, central Urals (Russia), Ore geology rew., 33: 20-30.
Zhou, M. F., Robinson, P. T., Malpas, J. and Li, Z., 1996- Podiform chromitites in the Luobusa ophiolite (Southern Tibet): implications for melt–rock interaction and chromite segregation in the upper mantle. Journal of Petrology 37, 3–21.
Zhou, M. F. and Robinson, P. T., 1997- Origin and tectonic environment of podiform chromite deposits, Econ. Geol., 92: 259-262.
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