بررسی شیمی کانی بیوتیت در گرانیتوئید زرگلی، شمال غرب زاهدان

[1] صادقیان، م (1383) ماگماتیسم، متالوژنی و مکانیسم جایگزینی تودة گرانیتوئیدی زاهدان، رسالة دکتری، دانشگاه تهران، دانشکده علوم، 450 ص.

[2] قاسمی، ح. ا.، صادقیان، م.، کرد، م.، خانعلی­زاده، ع (1388) سازوکار شکل­گیری باتولیت گرانیتوئیدی زاهدان، جنوب­شرق ایران، مجله بلورشناسی و کانی­شناسی ایران، شماره 4 ،551-578.

[3] کشتگر، ش (1383) پترولوژی، ژئوشیمی و تحلیل ساخـتاری گرانیت‌های زرگلی (‌شمال­غرب زاهـدان‌)، پایان­نامه کارشناسی­ارشد، دانشگاه تهران، 161 ص.

[4]              Abdel-Rahman A. M (1994) Nature of biotites for alkaline, calk-alkaline and peraluminous magmas, Journal of Petrology 35, 525-541.

[5]              Anderson J. L., Smith D. R (1995) The effects of temperature and ƒO₂ on the Al-in-hornblende barometer, American Mineralogist 80, 549-559.

[6]              Camp V. E., Griffis, R. J (1982) Character, genesis and tectonic setting of igneous rocks in the Sistan Suture Zone, eastern Iran, Lithos 15, 221-239.

[7]              De Pieri R., JobstraibizerPadova (1983) Crystal chemistry of biotites from dioritic to granodioritic rock-types of Adamello Massif (Northern Italy), NeuesJahrbuch Miner. Abh. 148, 58-82.

[8]              Esmaeily D., Maghdour-Mashhour R (2009) Geochemistry of biotites from Boroujerdgranitoid complex, SSZ, Iran: A crucial factor for illustration petrogenesis and tectonomagmatic environment of host rock?, Geophysical Research Abstracts, vol.11. EGU 7980.

[9]              Foster M.D (1960) Interpretation of the composition of trioctahedral micas, United states Geological Survey Professional Paper 354-B 11-46

[10]Huaimin X., Shuwen D., Ping J (2006) Mineral chemistry, geochemistry and U-Pb SHRIMP zircon data of the Yangxinmonzonitic intrusive in the foreland of the Dabieorogen”, Science in China: Series D Earth Sciences 49, 684-695.

[11]Middelaar, W. T., Keith, J. D (1990) Mica chemistry as an indicator of oxygen and halogen fugacities in the CanTung and other W-related granitoids in the North American Cordillera, Geological Society of America, Special Paper,246, 205-220.

[12]Monuz J.L (1984) F-OH and CI-OH exchange in mica with application to hydrothermal ore deposits, Reviews in Mineralogy13 469-493.

[13]Nachit H., Lbhi A., Abia E.H., Ohoud M.B (2005) Discrimination between primary magmatic biotites, reequilibratedbiotites and magmatic biotites and neoformedbiotites, Geomaterials (Mineralogy), Geoscience 337 1415-1420.

[14]Rezaei-Kahkhaei M., Kananian A., Esmaeily D., Asiabanha A (2010) Geochemistry of the Zargoli granite: Implications for development of the Sistan Suture Zone, southeastern Iran, Island Arc 19, 259-276.

[15]Shabani A.T., Lalonde A.E., Whalen J.B (2003) Composition of biotite from granitic rocks of the Canadian Appalachian orogen: A potential tectonomagmatic indicator? The Canadian Mineralogis 41, 1381-1396.

[16]Spear J.A (1984) Micas in igneous rocks, In: Micas, Bailey S.W., (ed); Mineralogical Society of America Review in Mineralogy, 13 299-356.

[17]Streckeisen A (1976) To each plutonic rock its proper name, Earth Sci. Rev. 12, 1-33.

[18][18] Wones D. R., Eugster H. P (1965) Stability of biotite: experiment, theory, and application, The American Mineralogist 50, 1228-1272.

[19]Xianwu B., Ruizhong H., Hanley J.J., Mungall J.E., Jiantang P., Linbo S., Kaixing W., Yan S., Hongli L., Xiaoyan H (2009)  Crystallisation condition (T, P, ƒO₂) from mineral chemistry of Cu- and Au-mineralised alkaline intrusions in the Red River-Jinshajiang alkaline igneous belt, western Yunnan Province, china, Miner. Petrol., 96, 43-58.

[20]Yang W J., Wang L K., Zhang S L., et al (1986) Micas of the two series of granites in south China, Acta Mineral Sin (in Chinese), 6(4): 298-307.

[21]Yang X. M., Lentz D. R (2005) Chemical composition of rock-forming minerals in gold-related granitoid intrusions, southwestern New Brunswick, Canada: implications for crystallization conditions, volatile exsolution, and fluorine-chlorine activity, Contrib. Mineral. Petrol., 150, 287-305.