شیمی‌کانی و پتروژنزکرومیتیت‌های منطقه گلوانس، کمپلکس دگرگونی شرقی افیولیت خوی

1. امامعلی­پور، ع (1388) ژئوشیمی و محیط زمین­شناسی کرومیتیت­های ناحیه الند از مجموعه افیولیتی خوی، شمال باختر ایران. فصلنامه علوم زمین، شماره هشتادم، 47-56.

2. امامعلی­پور، ع (١٣٨٠) متالوژنی افیولیت خوی با نگرشی ویژه بر انباشته­های سولفوری درآتشفشانی­های زیردریایی قزل داش خوی. پایان نامه دکتری، دانشگاه شهید بهشتی، ٤٦٦ ص .

3. امامعلی­پور، ع (١٣٨٧) بررسی کانی­شناسی کانی­های فرعی وکمیاب همراه با نهشته­های کرومیت ناحیه خوی. مجله بلورشناسی و کانی­شناسی ایران، شماره چهارم، ٥٦٠-٥٧٠.

4. داوودی اصل، ه (1392) بررسی کانی­زایی و ژنزکرومیت در پریدوتیت­های کلوانس خوی (آذربایجان غربی). پایان نامه کارشناسی­ارشد، دانشگاه آزاد اسلامی واحد اهر، 106 ص.

5. عزیزی، ح (١٣٨0) پتـروگرافی، پترولوژی و ژئوشیمی سنگ­های دگرگونی خوی. پایان نامه دکتری، دانشگاه تربیت معلم تهران، 253 ص.

6. فریدآزاد، م (١٣٨9) پترولوژی و پتروگرافی سنگ­های اولترامافیک و مافیک دگرگونی در مجموعه افیولیتی خوی (شمال غرب ایران)، پایان نامه دکتری، دانشگاه تبریز، 215ص.

7. کنعانیان، ع.، عطایی، م.، میرمحمدی، م. ص.، امامعلی­پور، ع (1389) سنگ­شناسی، شیمی کانی و شـکل­گیری کرومیت­های الند و قشلاق، مجموعه افیولیتی خوی (شمال غرب ایران). مجله بلورشناسی و کانی­شناسی ایران، شماره سوم، 371-382.

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

[9] Azizi, H., Moinvaziri, H., Mohajjel, M., and Yagobpoor, A (2006) PTt path in metamorphic rocks of the Khoy region (northwest Iran) and their tectonic significance for cretaceous-tertiary continental collision. Journal of Asian Earth Sciences, 27: 1-9.

[10] Ballhaus, C (1998) Origin of podiform chromite deposits by magma mingling. Earth and Planetary Science Letters, 1: 185–193.

[11] Boudier, F., Nicolas, A (1985) Harzburgite and lherzolite subtypes in ophiolitic and oceanic environments. Earth and Planetary Science Letters, 76: 84–92.

[12] Büchl, A., Brügmann, G., Batanova, V.G (2004) Formation of podiform chromitite deposits: implications from PGE abundances and Os isotopic compositions of chromites from the Troodos complex, Cyprus. Chemical Geology, 208: 217– 232.

[13] Coleman, R.G (1977) Ophiolites: Ancient Oceanic Lilhosphere?. New York: Springer-Verlag, 229 p.

[14] Dike H.J. B Bullen T (1984) Chromian spinel as a petrogenetic indicator in abyssal and alpine - type pridotites and spatially associated lavas. Contribution to Mineralogy and Petrology, 86: 54-76.

[15]

 Droop, G.T.R (1987) A general equation for estimating Fe³⁺ concentrations in ferromagnesian silicates and oxides from microprobe analysis, using stoichiometric criteria. Mineralogical Magazine 51: 431-435.

[16] Hassanipak, A., and Ghazi, M (2000) Petrology, geochemistry and tectonic setting of the Khoy ophiolite, North West Iran: implications for Tethyan tectonics. Journal of Asian Earth Sciences, 18: 109-121.

[17] Ismail, S.A., Mirza, T.M., Carr, P.F (2010) Platinum-group elements geochemistry in podiform chromitites and associated peridotites of the Mawat ophiolite, northeastern Iraq. Journal of Asian Earth Sciences, 37: 31-41.

[18] Kamenetsky, V.S., Crawford, A.J., Meffre, S (2001) Factors controlling chemistry of magmatic spinel: an empirical study of associated olivine, Cr-spinel and melt inclusions from primitive rocks. Journal of Petrology, 42: 655-671.

[19] Kelemen, P.B., Dick, H.J.B., Quick, J.E (1992) Formation of harzburgite by pervasive melt/rock reaction in the upper mantle. Nature, 358: 635-641.

 [20]

 Khalatbari-Jafari, M., Juteau, T., Bellon, H., Whitechurch, H., Cotton, Jo., Emami, H (2004) New geological, geochronological and geochemical investigations on the Khoy ophiolites and related formations, NW Iran. Journal of Asian Earth Sciences, 23: 507-535.

[21] Khalatbari-Jafari, M., Juteau, T., and Cotton, J (2006) Petrological and geochemical study of the late cretaceous ophiolite of Khoy (NW Iran), and related geological formations. Journal of Asian Earth Sciences, 27: 465-502.

[22] Lago, B., Rabinowicz, M., Nicolas, A (1982) Podiform chromite ore bodies: a genetic model. Journal of Petrology, 23: 103-125.

[23] Leblanc, M., Violette, J.F (1983) Distribution of aluminum - rich and chromium - rich chromite pods in ophiolite peridotites. Economic Geology, 78: 293-301.

[24] Maurel, C., Maurel, P (1982) Étude expérimentale de la distribution de láluminium entre bain silicate basique et spinelle chromifère. Implications pétrogénétiques: teneur en chrome des spinelles. Bulletin de Minéralogie, 105: 197-202.

[25] Melcher, F., Grum, W., Simon, G., Thalhammer, T.V., Stumpel, E (1997) Petrogenesis of the ophiolitic giant chromite deposits of Kempirsai, Kazakhstan: a study of solid and fluid inclusions in chromite. Journal of Petrology, 38: 1419-1458.

[26] Monsef, I., Rahgoshay, M., Mohajjel, M., and Shafaii Moghadam, H (2010) Peridotites from the Khoy Ophiolitic Complex, NW Iran: Evidence of mantle dynamics in a supra-subduction-zone context. Journal of Asian Earth Sciences, 38: 105–120.

[27] Proenza, J.A., Gervilla, F., Melgarejo, J.C., Bodinier, J.L (1999) Al- and Cr-rich chromitites from the Mayarí-Baracoa Ophiolitic Belt (Eastern Cuba): consequence of interaction between volatile-rich melts and peridotites in suprasubduction mantle. Economic Geology, 94: 547-566.

[28] Radfar, J. Amini, B. Behrudi, A. Khalatbari, M (1993) Geological map of the Khoy Quadrangle, Scale 1/100000. Geological Survey of Iran.

[29]

 Roberts, S., Neary, C.R (1993) Petrogenesis of ophiolitic chromitite. In: Prichard, H. M., Alabaster, T., Harris, N. B. W. & Neary, C. R. (eds) Magmatic Processes and Plate Tectonics, Geological Society Special Publication, 76: 257-294.

 [30] Rollinson, H (2008) The geochemistry of mantle chromitites from the northern part of the Oman ophiolite: inferred parental melt compositions. Contribution to Mineralogy and Petrology, 156: 273- 288.

[31] Rollinson, H.R (2005) Chromite in the mantle section of the Oman ophiolite: a new genetic model. Island Arc. 14: 542–550.

[32] Schiano, P., Clocchiatti, R., Lorand, J. P., Massare, D., Deloule, E., Chaussidon, M (1997) Primitive basaltic melts included in podiform chromites from the Oman ophiolite. Earth and Planetary Science Letters, 146: 489-497.

[33] Sisir, K.M., Edward M.R., Chusi L., Robert F (2006) The genesis of Archaean chromitites from the Nuasahi and Sukinda massifs in the singhbhum Craton, India. Precambrian Research, 148: 45-66.

[34] Uysal, I., Sadiklar, M.B., Tarkian, M., Karsli, O., 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.

[35]Zhou, M.F., Bai, W.j (1992) Chromite deposits in China and their origin. Mineralium Deposita 27: 192-199.

[36] Zhou, M.F., Robinson, P.T., Bai, W.j (1994) Formation of podiform chromitites by melt/ rock interaction in the upper mantle. Minerlium Deposita, 29: 98-101.

[37] Zhou, M.F., Robinson, P.T., Malpas, J., Li, Z (1996) Podiform Chromities in the Luobusa ophiolite (southern Tibet): Implications for melt-rock interaction and chromite segregation in the upper mantle. Journal of Petrology, 37: 3-21.

 [38] Zhou, M.F., Sun, M., Keays, R.R., Kerrich, R.W (1998) Controls on platinum-group elemental distributions of podiform chromitites: a case study of high-Cr and high-Al chromitites from Chinese orogenic belts. Geochimica et Cosmochimica Acta, 62: 677-688.