کانی شناسی، دما- فشار سنجی و تعیین زنجیره ماگمایی سنگهای آتشفشانی کوه دم، اردستان

[1] Technoexport., "Geological of the Anarak area (CENTRAL IRAN)", Geological survey of Iran, Report. TE/NO 19, (1984) 143.

[2] نبوی م. ح.، هوشمند زاده ع.، "نقشه 1:100000 کوه دم"، انتشارات سازمان زمین‌شناسی و اکتشافات معدنی کشور، (1354).

[3] شرکت مهندسین مشاور پیچاب کاوش، "مطالعات طرح اکتشافات نیمه تفضیلی طلای کوه دم اردستان"، انتشارات اداره کل معادن و فلزات استان اصفهان، (1379) ص 200 .

[4 شاهزیدی م.، "پترولوژی و پتروژنز توده ولکانیکی کوه دم واقع در اردستان، شمال شرقی استان اصفهان"، پایان نامه کارشناسی ارشد، (1385) ص 123.

[5] Deer W.A., Howie R.A., Zussman J., "An Introduction to the rock-forming minerals", Longman, (1991) 528.

[6] Best M.G., "Igneous and metamorphic petrology", Freeman and Company, (1982) 630.

[7] Morimoto N., Fabrise J., Ferguson A., Ginzburg I.V., Ross M., Seifert F.A., Zussman J., Akoi K., Gottardi G., "Nomenclature of pyroxenes", Mineral. Magazine 52, (1988) 535- 55.

[8] Deer W.A., Howie R.A., Zussman J., "Rock-forming minerals, (2nd ed), Single-Chain Silicates", Longman London, (1987) 668.

[9] Zhu Y., Ogasawara Y., "Clinopyroxene phenocryst from the Kokchetav shoshonitic volcanic rocks: Implications for the multi-stage magma processes", UHPM Workshop 2001 at Waseda University, (2001) 170-173.

[10] Deer W.A., Howie R.A., Zussman J., "An introduction to rock-forming minerals", Longman, (1965) 528.

11 Foster., "Classification diagram for biotite", Jour. Petrol 1, (1960).

[12] Peccerillo A., Taylor S.R., "Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu Area, Northern Turkey", Ibid 58, (1976) 63-81.

[13] Henry D.J., "Sulfide-silicate relations of the staurolite grade politic schists, Rangeley quadrangle", Maine. Ph.D. Thesis, University of Wisconsin-Madison Madison Wisconsin, (1981).

[14] Tronnes R.G., Edgar A.D., Arima M., "A high pressure-high temperature study of TiO2 solubility in Mg-rich phlogopite: Implications to phlogopite chemistry", Geochim. Cosmochim. Acta 49, (1985) 2323-2329.

[15] Arima M. and Edgar A. D., "Substitution mechanisms and solubility of titanium in phelogopite from rocks of probable mantle origin", Contrib. Mineral. Petrol 77, (1981) 288-295.

[16] Hall A., "Igneous Petrology (2nd ed)", Longman New York, (1996) 537.

[17] Shelley D., "Igneous and metamorphic rocks under the microscope", Chapman and Hall, (1993) 405.

[18] Nachite H., "Contribution a l e´ tude analytique et experimental des biotites des granitoids applications typologiques", These de Doctorat De L’ univesite´ de Bretagne accidental, (1986) 236.

[19] Abdel – Rahman A.M., "Nature of biotites from alkaline, Calc-alkaline and peraluminous magmas", J. Petrol 35, (1994) 525 – 541.

[20] Patino Douce A.E., "Titanium substitution in biotite: an empirical model with applications to thermometry, O2 and H2O barometries, and consequences form biotite stability", Chemic. Geol. 108, (1993) 133-162.

[21] LeBas N.J., "the role of aluminous in igneous clinopyroxenes with relation to their parentage", Am. Jour. Sci 260, (1962) 267 – 88.

[22] Leterrier J., Maury R.C., Thonon P., Girard D., Marchal M., "Clinopyroxene composition as a method of identification of the magmatic affinities of paleo-volcanic series", Earth. Planet. Sci. Lett 59, (1982) 139 – 154.

[23] Nisbet E.G., Pearce J.A., "Clinopyroxene compositions in mafic lavas in different tectonic settings", Contrib. Mineral. Petrol. 63, (1977) 149-160.

[24] Pe-piper G., "The Cenozoic volcanic sequence of Lesbos", Greece. Z. dt. Geol. Ges 131, (1980) 889-901.

[25] Schweitzer E.L., Papike J.J., Bence A.E., "Statistical analysis of clinopyroxenes from deep-sea basalts", Am. Mineral. 64, (1979) 501–13.

[26] Marcelot G., Maury R.C., Lefevre C., "Mineralogy of Erromango lava New Hebrides, Evidence of an early stage of fractionation in island arc basalts", Lithos 16, (1983) 135 – 151.

[27] Wass S.Y., "Multiple origins of clinopyroxenes in alkali basaltic rocks", Lithos 12, (1979) 115-132.

[28] Nimis P., Taylor W.R., "Single clinopyroxene Thermobarometery for garnet peridotites. Part I. Calibration and testing of the Cr-in-Cpx barometer and an enstitite-in-Cpx thermometer", Contrib. Mineral. Petrol 139, (2000) 541-554.

[29] Foley S.F., Venturelli G., "High K2O rocks with high MgO, High SiO2 affinities. In: Crawford, A.J., (ED.) Boninites and Related Rocks", Unwin Hyman London, (1989) 72-88.

[30] Liu T.C., Chen B.R., Chen C.H., "Melting experiment of a Wannienta basalt in the Kuanyinshan area, northern Taiwan", Jour. Asian. Earth. Sci 18, (2000) 519-531.

[31] Green D.H., Ringwood A.E., "The genesis of basaltic magmas", Contrib. Mineral. Petrol 15, (1967) 103-190.

[32] Aoki K., Shiba I., "Pyroxcene from lherzolite inclutions of Itinomegata, Japan", Lithos 6, (1973) 41-51.

[33] Helz R.T., "Phase relations of basalts in their melting range at PH2O= 5 kb as a function of oxygen fugacity", Jour. Petrol 17, (1973) 139-193.





[34] Brown W.L., and Parsons I., "Towards a more practical two – feldspar geothermometer", Contrib. Mineral. Petrol 76, (1981) 369 – 377.

[35] Seck H.A., "Koexistierende Alkalifeldspar and Plagioclase in system NaAlSi3O8– CaAlSi2O8–KalSi3O8– H2O bei temperature von 650C bis 900C", Neues Jahrbuch fur Mineralogie Abhundlungen 115, (1971) 315 – 345.

[36] Tuttle O.F., Bowen N.L., "Origin of granite in the light of experimental studies in the system NaAlSi3O8 – KalSi3O8 – SiO2 – H2O", Geol. Soc. Am. Men 74, (1958).

[37] Watson E.B., Harrison T.M., "Zircon thermometer reveals minimum melting conditions on earliest", Earth. Sci 38, (2005) 841-844.

[38] Lindsley D.H., Andersen D.J., "A two-pyroxene thermometer. Proceedings of the thirteenth Lunar and Planetary Science Conference, Part 2", Jour. Geophys. Res 88 Supplement, (1983) A887-A906.

[39] Jiang Y.H., Jiang S.Y., Ling H.F., Dai B.Z., "Low-degree melting of a metasomatized lithospheric mantle for theorigin of Cenozoic Yulong monzogranite-porphyry, east Tibet: Geochemical and Sr–Nd–Pb–Hf isotopic constraints", Earth .Planet. Sci. Lett 241, (2006) 617–633.

[40] Jahern J.S., Aaggarad P., "Compositional variations in diagenetic chlorites and illites, and relationships with formation-water chemistry", Clay Mineral 24, (1989) 157-170.

[41] Cathlineau M., "Cation site occupancy in chlorite and illite as a function of temperature",

Clay mineral 23, (1988) 471 – 485.