منابع
[1] اجاقی، ب (1374) زمینشناسی کانسار طلای زرشوران، مهندسین مشاور کاوشگران، گزارش داخلی، 165 صفحه.
[2] باباخانی،ع. ر.، قلمقاش، ج (1380) گزارش زمینشناسی 1:100000ورقه 1:100000چهارگوش تخت سلیمان، انتشارات سازمان زمینشتاسی و اکتشافات معدنی کشور، تهران، 110 صفحه.
[3] علــوینائیـنی، م.، و عمـیدی، م (1361) گــزارش زمینشناسی ورقه 1:250000 چهارگوش تکاب-صائین قلعه، انتشارات سازمان زمینشناسی و اکتشافات معدنی کشور، تهران، 100 صفحه.
[4] قربانی، م (1379) ماگماتیسم و متالوژنی منطقه تکاب، پایاننامه دکتری، دانشگاه شهید بهشتی تهران، 400 صفحه.
[5] Afzal, P. Fadakar Alghalandis, Y. Khakzadو A. Moarefvand,P, Rashidnejad Omran, N )2011( Delineation of mineralization zones in porphyry Cu deposits by fractal concentration–volume modeling. Journal of Geochemical Exploration, Vol.(108):220–232.
[6] Agterberg, F.P (1995) Multifractal modeling of the sizes and grades of giant and supergiant deposits. International Geological Review,37:1–8.
[7] Agterberg, F.P. Cheng, Q.& Wright, D.F (1993) Fractal modeling of mineral deposits. In: Elbrond J, Tang, X (eds) 24th APCOM symposium proceeding, Montreal, Canada, pp. 43–53.
[8] Carranza, E.J.M (2008) Geochemical Anomaly and Mineral Prospectivity Mapping in GIS. Handbook of Exploration and Environmental Geochemistry, Vol.(11). Amsterdam: Elsevier.
[9] Cheng, Q., Agterberg, F.P., Ballantyne, S.B (1994) The separation of geochemical anomalies from background by fractal methods. Journal of Geochemical Exploration, 51:109–130.
[10] Cheng, Q. & Agterberg, F.P (1996) Multifractal modeling and spatial statistics. Mathematical Geology,28:1–16.
[11] Cheng, Q. Ping, Q. &Kenny, F )1997( Statistical and fractal analysis of surface stream patterns in the Oak Ridges Moraine, Ontario, Canada. International Association of Mathematica lst Geology Meeting, Barcelona, Spain.
[12] Deng, J. Wang, Q. Yang, L. Wang, Y. Gong, Q.& Liu, H (2010) Delineation and explanation of geochemical anomalies using fractal models in the Heqing area, Yunnan Province, China.Journal of Geochemical Exploration,105: 95–105.
[13] Ford, A. & Blenkinsop, T.C (2008) Evaluation geological complexity and complexity gradients as control on copper mineralization, Mt Isa Inlier. Australian Journalof Earth Science,55:13-23.
[14] Gałuszka A (2007) A review of geochemical background concepts and an example using data from Poland.
[15] Jian, B. Porwal, A. Hart, C. Ford, A. &Yu, L )2010( Mapping geochemical singularity using multifractal analysis: application to anomaly definition on strean sediments data from Funin Sheet, Yunnan, China. Journal of Geochemical Exploration, 45:1-11.
[16] Mandelbrot, B (1983) The fractal geometry. Freeman and Company, New York. 468 pp .
[17] Mehrabi, B. Yardley, B. & Cann, J(1999) Sediment-hosted disseminated gold mineralisation at Zarshuran, NW Iran. Mineralium Deposita, 34, 673-696.
[18] Miesch, A (1981) Estimation of the geochemical threshold and its statistical significance.Journal of Geochemical Exploration, 16:49–76.
[19] Nazarpour, A. Omran, N.R. Paydar, G.R. Sadeghi, B. Matroud, F. & Nejad, A.M (2015) Application of classical statistics, logratio transformation and multifractal approaches to delineate geochemical anomalies in the Zarshuran gold district, NW Iran. Chemie der Erde-Geochemistry, 75, 117-132.
[20] Shapiro, S.S. & Wilk, M.B (1965) An analysis of variance test for normality (complete samples). Biomet, 52: 591–611.
[21] Yuan, F. Li, X.H. Bai, X.Y. Jowitt, S. Zhang, M. Jia, C.& Zhou, T (2010) Comparison of normalization methods for non-normal distributed soil geochemical data: a case study from the Tonglingmetallogenic district, Yangtze belt, Anhui Province, China. Journal of Geochemical Exploration,45: 45-51.
)