S Enayati Kolaie; M Yazdi; M.A.A Mokhtari
Abstract
Tazeh-Kand Cu mineralization area is located in ~20 km northeast of Tabriz, eastern Azarbaijan province. The area is a part of Central Iranian geo-structural zone in the eastern margin of the Tabriz 1:100000 geological map. Lithological units in this area composed of green- grey sandstones (redox zone), ...
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Tazeh-Kand Cu mineralization area is located in ~20 km northeast of Tabriz, eastern Azarbaijan province. The area is a part of Central Iranian geo-structural zone in the eastern margin of the Tabriz 1:100000 geological map. Lithological units in this area composed of green- grey sandstones (redox zone), red sandstones and marl (oxidized zone), salt domes and conglomerate (Miocene) along with dacitic domes (Pliocene). Based on petrographical investigations, the host sandstones are sub- mature to immature lithic arkos and were deposited in a tidal environment. Cu mineralization in this area occurred as stratiform type within the redoxed sandstones. The thickness of mineralized horizons vary between 30cm to 1m which are crops out up to 500m in some horizons. Concentration of Cu mineralization has direct relation with organic matter concentration. Mineralized horizons composed of three zones include: mineralized redox zone, bleached zone and red oxidized zone. Mineralogical investigations show that this mineralization composed of primary sulfide minerals include pyrite, chalcocite and digenite along with supergene minerals include covellite, malachite and Fe- hydroxides. Texturally, these minerals present as lenticular, disseminated, replacement, inter- grain cement and solution seems textures. According to petrographical and mineralogical results such as pyrite and primary chalcocite bearing redox sandstone, structural and textural evidences, stratigraphy, mineralization controlling factors, presence of organic matter as a redox material, permeability of host rock and salt diapirism, mineralization in the Tazeh-Kand area is mostly similar to RedBed type mineralization which is formed during the early to late diagenesis.
A Maghsoudi; M Vanaei; M Vanaei
Abstract
The NekaRiver is located at 21km in east of Sari, center city of the Mazanderan province, north of Iran. 51 stream sediment samples were collected from 4 sample sites. The samples were digested by HF+HClO4+HNO3 and analyzed by AAS in laboratory of Geological Survey of Iran. The results of analysis show ...
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The NekaRiver is located at 21km in east of Sari, center city of the Mazanderan province, north of Iran. 51 stream sediment samples were collected from 4 sample sites. The samples were digested by HF+HClO4+HNO3 and analyzed by AAS in laboratory of Geological Survey of Iran. The results of analysis show that the enrichment ratio and Geo-accumulation index are too high for Ag, Cd and Sn in the whole sediments of the NekaRiver. Zn shows very high enrichment in the sites of Boz Mil and Lajan Lateh Sofla sample sites and Pb shows very high enrichment in the site of Boz Mil. Degrees of Geo-accumulation Index are very high for Ag-Cd in the 4 sites but for Zn are high to medium and for other elements are medium. In the Neka Choob and Mola Khil sample sites, the Co and Ag are too high because of anthropogenic contamination and Fe and Ni are low relatively. In the Boz Mil and Lajan Lateh Sofla sample sites, the Pb and Ag are too high because of anthropogenic contamination and V, Ni, Cu and Zn are low relatively. Coal mining and coal deposition in the upper part of the NekaRiver, urban and wood industry sewage are the main sources of the pollution.
