Petrography of plutonic rocks in the late cambrian (rizu series), se-chahun iron oxide deposite, bafq mining district, Central Iran
Paper Details
Petrography of plutonic rocks in the late cambrian (rizu series), se-chahun iron oxide deposite, bafq mining district, Central Iran
Abstract
The iron ore deposits of the Bafq district are associated with volcano sedimentary rocks and shallow depth intrusions. The Se–Chahun Iron Ore mine is containing two major groups of ore bodies called the X and XI anomalies. One of the important plutonic rocks in the study area is Narigan granites have two type; first type granite is white to gray leucogranite with a different grain size and second type granites are a pale-pink and have a medium-grained size. Second type of granite is intruded between first type granites and the study of textures show that first type granite is formed in deeper levels. Other important litho-type is Pyroxene gabbros, in the thin section this rocks contain plagioclase (Alb) anhedral pyroxene (augite). That is crystallized between plagioclase spaces and has an ophitic texture.
NISCO, 1975. “The results of the geological prospecting at the Chador Malu deposit”. Unpubl Rept. National Iranian Steel Corporation. 57 p.
Samani B. 1988. Metallogeny of the Precambrian in Iran. Precamb. Res. 39, 85–106.
Barton MD, Johnson DA. 1996. Evaporitic source model for igneous-related Fe oxide- (REE-Cu-Au-U) mineralization. Geology 24, 259–262.
Bonyadi Z, Davidson GJ, Mehrabi B, Meffre S, Ghazban F. 2010. Significance of apatite REE depletion and monazite inclusions in the brecciated Se-Chahun iron oxide-apatite deposit, Bafq district, Iran: Insights from paragenesis and geochemistry. Chemical Geology 281, 253-269.
Daliran F. 2002. Kiruna-type iron oxide-apatite ores and ‘apatites’ of the Bafq district, Iran, with an emphasis on the REE geochemistry of their apatites. In: Porter, T.M. (Ed.), Hydrothermal Iron Oxide Copper gold & Related Deposits: A GlobalPerspective, volume 2. PGC Publishing, Adelaide, Australia, 303–320.
Haghipour A, Valeh N, Pelissier G, Davoudzadeh M. 1977, Explanatory text of the Ardekan quadrangle map, 1:250,000, Geological Survey of Iran, H8, 114 p.
Jami M. 2005. Geology, Geochemistry Esfordi Phosphate – Iron Deposit, Bafq Area, Central Iran and Evolution of the. PhD thesis. The University of new South wallets.
Jami M, Dunlop AC, Cohen DR. 2007. Fluid Inclusion and Stable Isotope Study of the Esfordi Apatite-Magnetite Deposit, Central Iran. Journal of Economic geology. 102, 1111–1128.
Ramezani J. 1997. Regional geology, geochronology and geochemistry of the igneousand metamorphic rock suites of the Saghand Area, central Iran: Unpublished Ph.D. thesis, St. Louis, Missouri, Washington University, 416 p.
Samani B. 1993. ”Saghand formation, a riftogenic unit of precambrian in Central Iran”, Geoscience, 2(6), 32-45. Geological Survay Iran.
Stosch HG, Romer RL, Daliran F, Rhede D. 2011. Uranium–lead ages of apatite from iron oxide ores of the Bafq district, east-Central Iran. Mineralium Deposita 9–22.
Torab FM. 2008. Geochemistry and metallogeny of magnetiteapatite deposits of the Bafq Mining District, Central Iran. PhD thesis. Clausthal University of Technology.
Torab FM, Lehmann B. 2007. Magnetite-apatite deposits of the Bafq district, Central Iran: apatite geochemistry and monazite geochronology. journal of Mining. 71, 347–363.
Williams PJ, Barton MD, Fontboté L, de Haller A, Johnson DA, Mark G, Marschik R, Oliver NHS. 2005. Iron-oxide-copper-gold deposits: Geology, space-time distribution, and possible modes of origin. Economic Geology 100th Anniversary Volume, 371–406.
Zahra Hossein Mirzaei Beni, M.H. Emami, S. J. Sheikhzakariaee, A. Nasr Esfahani (2014), Petrography of plutonic rocks in the late cambrian (rizu series), se-chahun iron oxide deposite, bafq mining district, Central Iran; JBES, V5, N4, October, P610-616
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