[1] نادری ن.، " نقشهی زمینشناسی 1:100000 کدکن"، انتشارات سازمان زمینشناسی و اکتشافات معدنی کشور (1377).
[2] میرا و.، "اکتشافات ژئوشیمیایی و زمینشناسی اقتصادی رگههای طلای هیدروترمال منطقه ارغش (نیشابور)". پایاننامه کارشناسی ارشد، دانشگاه شهید بهشتی تهران، (1378) 181ص.
[3] بیات ع.، "تعیین ژنزومدلسازی ترمودینامیکی کانسار طلای ارغش با مطاله سیالات درگیر". پایاننامه کارشناسی ارشد، دانشگاه صنعتی امیر کبیر، دردست اجرا، (1387).
[4] Ishihara S., "The magnetite-series and ilmenite-series granitic rocks": Mining geology, Japan, 27, 1977, p.43-300.
[5] Chappel B.w., White A.J.R., Braynt C.J., Wyborn D., Williams I.S., Recourse Geology, V. 48, No. 4,(1988) p. 225-235.
[6] کریمپور م.ح.، ملکزاده آ.، حیدریان م.ر.، "اکتشاف ذخایر معدنی، مدلهای زمینشناسی، ژئوشیمی، ماهوارهای و ژئوفیزیکی"، دانشگاه فردوسی مشهد، (1384) صص 188- 316.
[7] Creasey S.C. "Some phase relations in hydrothermally altered rock of porphyry copper deposits": Econ. Geol., 54, (1959) 351-373.
[8] Carson D.J.T., Jambor J.L., "Mineralogy, zonal relationships and economic significance of hydrothermal alteration at porphyry copper deposits", Babine Lake area, British Columbia: Canadian Institute of Mining and Metallurgy Bulletin, v. 76,( 1974) p. 24.
[9] Barnes H., "Geochemistry of hydrothermal ore deposits", Holt, Rinehart and Winston, (1967) p.670.
[10] Philips W. M., Revell Griffen, Dana T., "Optical Mineraligy, Freman and Company", (1981) p. 688.
[11] Ossandon G., Freraut R., Gustafson L.B., Lindsay D.D., Zentilli M., "Geology of the Chuquicamata mine: a progress report". Economic Geology 96: (2001) 249-270.
[12] Eshaghpour M., "Borehole Geology and Alteration Mineralogy of Well NWS-4, Mt.Sabalan Geothermal Field,NW-Iran", Proceedings World Geothermal Congress, Antalya, Turke (2005).
[13] Carson D.J.T., Jambor J.L., "The occurrence and significance of phyllic overprinting at porphyry copper-molybdenum deposits (abstract)", Canadian Institute of Mining and Metallurgy, v. 72,( 1979) p. 78.
[14] Eckstrand O.R., "The crystal chemistry of chlorite: unpublished Ph.D. thesis", Harvard university (1963).
[15] Bowen R., Gunatilaka A., "Copper: it’s geology and economics", Applied sciences published Ltd, London,( 1977) pp. 12-158.
[16] کوثری س.، "گزارش عملیات اکتشافی در کانسار طلای ارغش- کانسارطلای شماره2- جنوبغرب نیشابور(فازدوم)"، سازمان زمینشناسی و اکتشافات معنی کشور، (1382).
[17] Hunt J.P., "Porphyry copper deposits; in Hutchinson", R.W., and Grauch, R.I., eds., Historical Perspectives of Genetic Concepts and Case Histories of Famous Discoveries: Economic Geology Monograph 8, (1991) p. 192-206.
[18] Waterman G. C., Hamilton R. L., "The Sar
Cheshmeh porphyry copper deposit", Economic
Geology, v.70,no.3, (1975) p. 568-576.
[19] Carten R.B., Geraghty E.P., Walker B.M., "Cyclic development of igneous features and their relationship to high-temperature hydrothermal features in the Henderson porphyry molybdenum deposit", Colorado: Economic Geology, v. 83, (1988) p. 266-296.
[20] Heidrick T.L., Titley S.R., "Fracture and dike patterns in Laramide plutons and their structural and tectonic implication: American Southwest", in Titley, S.R., ed., Advances in Geology of the Porphyry Copper Deposits, Southwestern North America: University of Arizona Press, Tucson, Arizona, (1982) p. 73-91.
[21] Linnen R.L., Williams-Jones A.E., "Tectonic control of quartz vein orientations at the Trout Lake stockwork molybdenum deposit, southeastern British Columbia: Implications for metallogeny in the Kootenay Arc", Economic Geology, v. 82, (1987) p.1283-1293.
[22] Rehrig W.A., Heidrick T.L., "Regional fracturing in Laramide stocks of Arizona and its relationship to porphyry copper mineralization", Economic Geology, v. 67, (1972) p. 198-213.
)