Kharazmi Journal of Earth Sciences

Kharazmi Journal of Earth Sciences

Geology, geochemistry and iron mineralization in the Qazikandi area, NW of Zanjan

Authors
1 University of Zanjan
2 Institute for Advanced Studies in Basic Sciences (IASBS)
3 Sadr Jahan Mines Devolapment Company, Tehran, Iran
Abstract
The Qazikandi iron ore mineralization is located in the 70 km northwest of Zanjan and belongs to the Central Iran Zone. The rock units in the study area include Precambrian to Cenozoic formations as well as Cretaceous granite bodies. Iron mineralization in the Qazikandi area has occurred in the form of lensoid and vein in the basal part of the Barout Formation with carbonate and shale composition. The main ore minerals consist of magnetite, primary hematite, pyrite, secondary hematite and goethite. The secondary minerals which formed through supergene process and evolved during weathering of magnetite and pyrite are secondary hematite, goethite and lepidocrocite. The alteration in the study mineralization includes chloritization, epidotization, silicic, sericitization and argillic. The current research suggests that the intrusion of plutonic body with granite to quartz-monzonite composition into the Barout Formation has led to the formation of iron mineralization in the area. Due to the intrusion of the plutonic body into the shale parts of the Barout Formation, the hornfels developed and anhydrous minerals such as phlogopite were formed. Following the mineralization in this area, magnetite and then small amounts of primary hematite were formed. The mentioned alteration products developed simultaneously with this stage of mineralization. It is noteworthy that the silicic veins and veinlets which formed after mineralization, have cut the primary phases of mineralization. The field and microscopic evidence suggest that the Qazikandi ore deposit is classified as the magnesian skarn iron ore deposit.
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Boynton, W.V., 1984. Cosmochemistry of the earth element: meteorite studies, In: Henderson, R. (Ed), Rare Earth Element geochemistry. Developments in geochemistry, v. 2. Elsevier, Amsterdam.
Craig, J.R., Vaughan, D.L., 1994. Ore Microscopy and Ore Petrography, John Wiley and Sons, 440 p.
Chappell, B.W., White, A.J.R., 2001. Two contrasting granite types. 25 years later.
Australian Journal of Earth Sciences 48, 489-499.
Ghorbani, M., 2003. The economic geology of Iran, mineral deposits and natural resources. Springer Geology, doi:10.1007/978-94-007-5625-0, 569 p. Dordrecht.
Lotfi, M., 2001. Geological map of the Mahneshan, scale: 1:100000. Geological survey of Iran, Tehran, Iran.
Meinert, L.D., 1992. Skarns and skarn deposits. Geoscience Canada 19, 145-162.
Meinert, L.D., 1995. Compositional variation of igneous rocks associated with skarn deposits: chemical evidence for a genetic connection between petrogenesis and mineralization, In: Thompson, J.F.H. (Ed.), Magmas, Fluids and Ore Deposits. Mineralogical Association of Canada, Short Course Series 23, pp. 400-418.
Meinert, L.D., Brooks, J.W., Myers, G.L., 1990. Whole rock geochemistry and contrast among skarn-types, In Meinert, L.D. (ed.), Skarn deposits in Nevada, Great Basin Symposium, Geology and ore deposits of the Great Basin, Geological Society of Nevada, fieldtrip 2, Guide book, pp. 179-192.
Meinert, L.D., Dipple, G.M., Nicolescu, S., 2005. World skarn deposits, Economic Geology 100th Ann, 299-336.
Middlemost, E.A.K., 1985. Magmas and magmatic rocks: An introduction to igneous petrology, London, New York: Longman, 266p.
Newberry, R.J., Burns, L.E., Swanson, S.E., Smith, T.E., 1990. Comparative petrologic evolution of the Sn and W granites of the Fairbanks Circle area, interior Alaska, In Stein, H.J. and Hannah, J.L. (eds.), Ore-bearing granite systems: Petrogenesis and mineralizing processes. Geological Society of America, Special Paper, pp. 121-142.
Pearce, J.A., Harris, N.B., Tindle, A.G., 1984. Trace element discrimination diagrams for the Tectonic interpretation of granitic rocks. Journal of Petrology, 25(4), 956-983.
Peccerillo, A., Taylor, S.R., 1976. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, northern Turkey. Contribution to Mineralogy and Petrology 58(1), 63-81.
Pirajno, F., 2009. Hydrothermal processes and mineral systems. Springer, Berlin, Germany, 1250 p.
Rollinson, H.G., 1993. Using geochemical data: evaluation, presentation and interpretation. Longman Group UK Limited, London, 384 p.
Seedorf, E., Dilles, J.H., Proffett, J.M., Einaudi, M.T., Zurcher, L., Stavast, W.J.A., Johnson, D.A., Barton, M.D., 2005. Porphyry deposits: Characteristics and origin of hypogene features. Economic Geology 100th Ann, https://doi.org/10.5382/AV100.10
Shand, S.J., 1943. The Eruptive Rocks. Hafner Publishing Company, New York, John Wiley and sons, 444 p.
Srivastava, R.K., Singh, R.K., 2004. Trace element geochemistry and genesis of Precambrian sub-alkaline mafic dikes from the central Indian craton evidence for mantle metasomatism. Journal of Asian Earth Sciences 23, 373-389.
Sun, S.S., McDonough, W.F., 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. Geological Society, London, Special Publications 42(1), 313-345.
Whalen, J.B., Currie, K.L., 1987. Chappell, B.W., A-type granites: geochemical characteristics, distribution and petrogenesis. Contribution to Mineralogy and Petrology 95, 407–419.
Whitney, D.L. Evans, B.W., 2010. Abbreviations for names of rock-forming minerals. American Mineralogist 95, 185-187.
Wilson, M., 1989. Igneous petrogenesis: A global tectonic approach. Unwin Hyman Ltd, 466 p.
Zhou, L., Mab, C., She, Z., 2012. An Early Cretaceous garnet-bearing metaluminous A-type granite intrusion in the East Qinling Orogen, Central China: Petrological, mineralogical and geochemical constraints. Geoscience Frontiers 3(5), 635-646.