[1] Daliran F., “The carbonate rock-hosted epithermal gold deposit of Agdarreh, Takab geothermal field, NW Iran, hydrothermal alteration and mineralization”, Mineralium Deposita, 43 (2008) 383-404.
[2] Daliran F., Hofstra A.H., Walther J., Stüben D., “Aghdarreh and Zarshuran SRHDG deposits, Takab region, NW Iran’, GSA Annual Meeting, Abstract with Programs (2002) P.8-63.
[3] Mehrabi B., Yardley B. W. D., Cam J. R., “Sediment-hosted disseminated gold mineralization at Zarshuran, NW Iran”, Mineralium Deposita, 34 (1999) 673-696.
[4] Asadi H.H., Voncken J.H.L., Kühnel R.A., Hale M., “Petrography, mineralogy, and geochemistry of the Zarshuran Carlin-like gold deposit, northwest Iran”. Mineralium Deposita, 5 (2000) 656-671.
[5] Gilg H. A., Boni M., Balassone G., Allen C. R., Banks D., Moore F., “Marble-hosted sulphide ores in the Angouran Zn-(Pb-Ag) deposit, NW Iran: interaction of sedimentary brines with a metamorphic core complex”, Mineralium Deposita, 41 (2006) 1-16.
[6] Boni M., Gilg H.A., Balassone G., Schneider J., Allen C.R., Moore F., “Hypogene Zn carbonate ores in the Angouran deposit, NW Iran”, Mineralium Deposita, 42 (2007) 799-820.
[8] Karami F., Kouhestani H., Mokhtari M.A.A., Azimzadeh A.M., “The Halab deposit, SW Zanjan: Volcanogenic massive sulfide Zn–Pb (Ag) mineralization, Takab–Takht-e-Soleyman–Angouran metallogenic district”, Journal of Economic Geology 13(1) (2021) 165–192.
[9] Karbasi A., “final report of Halab zinc-lead exploration. Organization of Industry”, Mining and Trade of Zanjan Province (2014).
[10] Ghazvinizadeh A.M., “Genesis of Alamkandi Pb–Zn deposit, Zanjan Province. MSc. thesis, University of Kharazmi”, Tehran (In Persian with English abstract) (2005).
[11] Shirkhani M., “Mineralogy, geochemistry and genesis of Ay Qalasi Lead and Zinc deposit, south east of Takab”, M.Sc. thesis, Tarbiat Modares University (2008) 143 p.
[13] Mohmmadi Niaei R., Nezafati N., Ghorbani M., Sheikhzakariaei Daliran F., “Mineralogy and chemical variations of sulfosalts of epithermal deposit of Ay-Qalasi (southeast of Takab, northwest of Iran)”, Iranian Journal of Crystallography and Mineralogy, 30 (2)
[14] Heidari S.M., Daliran F., Paquette J.L., Gasquet D., “Geology, timing, and genesis of the high sulfidation Au (–Cu) deposit of Touzlar, NW Iran”, Ore Geology Reviews 65, 460-486.
[15] Najafzadeh M., Ebrahimi M., Mokhtari M.A.A., Kouhestani H., “Arabshah Mineral Occurrence: Carlin-Type Epithermal Gold-Arsenic-Antimony Mineralization in Takab-Angouran Metallogenic Zone, Takht Soleiman, West Azerbaijan”, Advanced Applied Geology, 25 (2015) 61-76.
[16] Talebi L., Mokhtari M.A.A., Ebrahimi M., Kouhestani H., “Arpachai Mineral Occurrence, North of Takab: Epithermal Mineralization of Base Metals in the Takab-Angouran-Takht Solaiman Metallogenic Zone”, Earth Sciences Quarterly . GSJ_Volume 26_Issue 104_Pages 281-296.
[17] Rahmati N., “Petrology and geochemistry of volcanic rocks in the Agh Otag area (N Takab) with considering Au-Cu mineralization”, M.Sc. thesis, University of Zanjan, Zanjan, Iran (in Persian) (2015).
[18] Pour Mohammad F., Kohestani H., Azimzadeh A.M., Nabatian Gh., Mokhtari M.A.A., “Mianaj iron occurrence, southwest of Zanjan: Metamorphosed and deformed volcano-sedimentary type of mineralization in Sanandaj- Sirjan zone”, Earth Sciences Quarterly. GSJ_Volume 28 (2018|) Issue 111_Pages 161-174.
[19] Mohammadi Z., Ebrahimi M., Kouhestani H., “Goorgoor Iron Occurrence, Northeast of Takab: Metamorphosed Volcano-Sedimentary Mineralization in Sanandaj- Sirjan zone”, Advanced Applied Geology, 13 (2013) 20-32.
[20] Nouri F., Mokhtari M.A.A., Izadyar J., Kouhestani H., “Geological and mineralogical characteristics of Alamkandi Fe deposit, west of Zanjan. The 35th symposium on geosciences”, Geological Survey of Iran (In Persian with English abstract) (2017).
[21] Maanijou M., Salemi R., “Mineralogy, chemistry of magnetite and genesis of Korkora-1 iron deposit, east of Takab, NW Iran”, Journal of Economic Geology, 6 (2014) 355–374 (in Persian with English abstract).
[22] Maanijou m., Khodaei L., “Mineralogy and electron microprobe study in Sarab-3 iron deposit, southwest of Shahrak mining area (east of Takab)”. Economic Geology, 10(1) (2017) 267-293.
[23] Nadari A., Nabatian Gh., Honarmand M., Kouhestani H., “Geology and genesis of Halab Mn deposit, SW Zanjan”, Earth Science Quarterly. GEOSCIENCES, Vol. 29 (2019) No. 115.
[24] Lotfi M., Karimi M., “Mineralization and formation of vein-type deposits (nickel-cobalt-arsenic-bismuth and basic elements) in Bayche- Bagh (Northwestern Zanjan - Iran)”, Journal of Earth Sciences, 53 (2013) 81-95.
[26] Agard Ph., Omrani J., Jolivet L., Whitechurch H., Vrielynck B., Spakman W., Monié P., Meyer B., Wortel M., “Zagros orogeny: A subduction-dominated process”, Geological Magazine 148 (2011) (5-6). DOI: 10.1017/S001675681100046X.
[27] Rajabi A., Rastad E., Canet C., “Metallogeny of Cretaceous carbonate-hosted Zn-Pb deposits of Iran: Geotectonic setting and data integration for future mineral exploration”, International Geology Review, 54(14) (2012) 1649-1672. DOI: 10.1080/00206814.2012.659110.
[28] Zhuang L., Song Y., Liu Y., Fard M., Hou Z., “Major and trace elements and sulfur isotopes in two stages of sphalerite from the world-class Angouran Zn–Pb deposit, Iran: Implications for mineralization conditions and type”, Ore Geology Reviews, 109 (2019) 184-200.
[29] Mohajjel M., “Structure and tectonic evolution of Palaeozoic–Mesozoic rocks, Sanandaj–Sirjan Zone, western Iran. Ph.D. Thesis, University of Wollongong”, Wollongong, Australia (unpublished) (1997) 226 p.
[30] Aghazadeh M., Castro A., Rashidnejhad Omran N., Emami M.H., Moinvaziri H., Badrzadeh Z., “The gabbro (shoshonitic)-monzonite- granodiorite association of Khankandi pluton, Alborz Mountains, NW Iran”, Journal of Asian Earth Science., 38 (2010)199–219.
[31] Hassanzadeh J., Wernicke B.P., “The Neotethyan Sanandaj-Sirjan zone of Iran is an archetype for passive margin-arc transitions”, Tectonics, 35 (2016) 586–621.
[32] Baghban S., Hosseinzadeh M.R., Moayyed M., Mokhtari M.A.A., Gregory D., Mahmoudi Nia H., “Chemical composition and evolution of the garnets in the Astamal Fe-LREE distal skarn deposit, Qara Dagh–Sabalan metallogenic belt, Lesser Caucasus, NW Iran”, Ore Geology Reviews, 78, 166–175.
[33] Hajialioghli R., Moazzen M., Oberhänsli R., Ahmadzadeh S., Ahangari M., “Back-arc Magmatism in the Cadomian Basin of NW Iran: Ortho-Amphibolites from the Alam-Kandi Area”, Geotectonics., 57 (2023) 200–212.
[34] Alavi M., Amidi M., “Geological map of the Takab Quadrangle, West Azerbaijan Province, Scale 1: 250000. Iran Geological Survey and Mineral Explorations .
[35] Daliran F., Pride K., Walther W., Berner Z.A., Bakker R.J., “The Angouran Zn (Pb) deposit, NW Iran: evidence for a two-stage, hypogene zinc sulfide–zinc carbonate mineralization”, Ore Geology Reviews, 53 (2013) 373-402.
[36] Whitney D.L., Evans B.W., “Abbreviations for names of rock-forming minerals. American Mineralogist”, Volume 95 (2010) pages 185–187.
[37] Babakhani A.R., Ghalamghash J., “Geological map of Takht-e-Soleyman, scale 1:100000”, Geological Survey of Iran.
[38] Fonoudi M., Hariri A., “Geological map of Takab, scale 1:100,000”, Geological Survey of Iran (1999).
[40] Meinert L.D., “Skarns and skarn deposits”, Geoscience Canada, 19(4) (1992) 145-162.
[41] Berman R.G., Brown T.H., Greenwood H.J., “An internally consistent thermodynamic database for minerals in the system Na2O-K2O-CaO-MgO-FeO-SiO2-Al2O3-Fe2O3-TiO2-H2O-CO2”,Atomic Energy of Canada Technical Report, TR-337, 62 p.
[42] Perkins E.H., Brown T.H., Berman R.G., “PTX-SYSTEM: Three programs for calculation of pressure- temperature-composition phase diagrams”, Comput Geoscience 12 (1986) 749–755.
[43] Advay M., Moazzen M., Hajialioghli R.,
“Geochemical features of amphibolites from the Qarehaghaj area, East Azerbaijan, NW Iran; implications for paleotectonic setting”, Neues Jahrbuch für Geologie und Paläontologie, 281(1) (2016) 35–49.
[44] Sorokin A.A., Ovchinnikov R.O., Xu W., Kovach V.P., Yang H., Kotov A.B., Ponomarchuk V.A., Travin A.V., Plotkina Y.V., “Ages and nature of the protolith of the Tulovchikha metamorphic complex in the Bureya Massif, Central Asian Orogenic Belt”, Russia: Evidence from U–Th–Pb, Lu-Hf, Sm-Nd, and 40Ar/39Ar data. Lithos, 332–333 (2019) 340–354.
[45] Spitz G., Darling R., “Major and minor element lithogeochemical anomalies surrounding the Louvem copper deposit, Vald’Or, Quebec”, Canadian Journal of Earth Sciences, 15 (1978) 1161–1169.
[46] Saeki Y., Date J., “Computer application to the alteration data of the footwall dacite lava at the Ezuri Kuroko deposits”, Akito Prefecture. Mining Geology, 30 (1980) 241–250.
[47] Jenner G.A., “Trace element geochemistry of igneous rocks: Geochemical nomenclature and analytical geochemistry. in: Wyman, D.A., ed., Trace Element Geochemistry of Volcanic Rocks: Applications for Massive Sulfide Exploration. Geological Association of Canada”, Short Course Notes, 12 (1996) 51–77.
[48] MacLean W.H., Kranidiotis P., “Immobile elements as monitors of mass transfer in hydrothermal alteration: Phelps Dodge massive sulfide deposit, Matagami, Quebec”, Economic Geology, 82 (1987) 951–62.
[49] MacLean W.H., Barrett T.J., “Lithogeochemical techniques using immobile elements”, Journal of Geochemical Exploration, 48 (1993) 109–33.
[50] Wood D.A., “The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary volcanic province”, Earth and Planetary Science Letters, 50 (1980) 11-30.
[51] Cabanis B., Lecolle M., “Le diagramme La/10-Y/15-Nb/8: un outfil pour la discrimination de series volcaniques et lamise en evidence des processus demélange et/ou de contamination crustale”, Compte Rendus de I’Académie des Sciences (Ser. II) 309 (1989) 2023–2029.
[52] Pearce J.A., “Role of the sub-continental lithosphere in magma genesis at active continental margins. In: Hawkesworth, C.J., Norry, M.J. (eds)”, Continental Basalts and Mantle Xenoliths. Nantwich UK Shiva (1983) pp. 230-249.
[53] Bonin B., “From orogenic to anorogenic settings: Evolution of granitoid suites after a major orogenesis”, Geological Journal, 25(3-4),, 261-270
[54] Cox, D.P., Singer, D.A., 1986. Mineral deposit models. US Geological Survey Bulletin 1693 (1990) p. 379.
[55] Dill H.G., “The chessboard classification scheme of mineral deposits: mineralogy and geology from aluminum to zirconium”, Earth-Science Reviews, 100 (1–4) (2010) 1–20.