Gradation and geochemistry of the Fenced Lagoon sediments (Bandar Anzali) with regard to source rock and tectonic location
Keywords:
Anzali port, sediment, sedimentary geochemistry, measurement of metals, origin, tectonic location
Abstract
The location of the Fenced Lagoon in the urban basin of Bandar Anzali, which should be considered due to its impact on the lives of the people of the region in terms of the conservation of the wetland and its environmental issues, and, on the other hand, the potential of this area to be introduced as a geotourism center determine the need to investigate the area’s sedimentology and geochemistry. Therefore, to study sedimentary and geochemical properties of the Fenced Lagoon sediments located in Bandar Anzali, 33 samples were taken in the form of 6 cores and 12 grabs, and basic sedimentation tests and heavy metals measurement were carried out on them .Studies show that the sediments range from sand to clay in terms of gradation and have mainly coastal-river origin. The sediments of this lake are classified into four sedimentary types: Muddy Sand, Slightly Gravelly Muddy Sand, Sand and Slightly Gravelly Sand, and sand is the main component of all of these sediments. The most abundant sedimentary types belong to Muddy Sand and Sand and the least abundant sedimentary types belong to Slightly Gravelly Muddy Sand and Slightly Gravely Sand. The nature of the source rock is derived from acidic to intermediate combination and in general, sedimentary rocks of the area under study are within the continental arch islands and, to a lesser extent, the active continental margin.References
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27. Ghazban, F., Zare, M., 2011, Survey of the origin of heavy metals pollution in Bandar Anzali sediments (North Of Iran), Environmental sciences, thirty and seventh year, No. 57, Spring 2011, P: 45 – 56.
28. Glazovski N.F., 1991, The Aral Crisis. Source, Current Situation and Way Out, Artobolevskiy S.S., Kuklin’ ski A., «USSR in the Perspective of Global Change,» pp. 167-199, Polish Association for the Club of Rome, Warsaw, Globality versus Locality, vol. 3.
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31. Hayashi, K. I., Fujisawa, H., Holland, H. D. & Ohmoto, H., 1997. Geochemistry of approximately 1.9 Ga sedimentary rocks from northeastern Labrador, Canada. GeochimCosmochimActa, v.61, 4115-4137.
32. Jansen, J.H.F., Van der Gaast, S.J., Koster, B., Vaars, A.J., 1998. CORTEX, a shipboard XRF-scanner for element analyses in split sediment cores. Mar. Geol. 151, 143–153.
33. Jin, Z., Li, F., Cao, J., Wang, S. & Yu, J., 2006. Geochemistry of Daihai Lake sediments, Inner Mongolia, north China: Implications for provenance, sedimentary sorting and catchment weathering. Geomorphology, v.80, p.147-163.
34. Kakroodi, A. A., S. B. Kroonenberg, R. M. Hoogendoorn, H. MohammdKhani, M. Yamani, M. R. Ghassem i& H. A. K. Lahijani, 2012b, Rapid Holocene sea level changes along the Iranian Caspian coast. Quaternary International, 263: 93-103.
35. Kazanci, N.; Türkmen, G.; Ertunç, Ö.; Gültutan, Y.; Ekingen, P.; Öz, B., 2008b. A research on water quality of Kelkit stream using benthic macroinvertebrates and physicochemical variables, Rev. Hydrobio., 1 (2), 145-160 (16 pages).
36. Karageorgis, A.; Anagnostou, Ch.; Sioulas, A.; Chronis, G.; and Papathanassiou, E: 1998. Sediment geochemistry and mineralogy in Milos Bay. SW Kyklades. Aegean Sea. Greece. Journal of Marine Systems. 16: 269-281.
37. Katemaunzanga, D., and Gunter, 2009.Lithostratigraphy, Sedimentology, and Provenance of the Balfour Formation (Beaufort Group) in the Fort Beaufort– Alice Area, Eastern Cape Province, South Africa, ActaGeologicaSinica (English Edition), Volume 83, Issue 5, October 2009, 902–916.
38. Lahijani, H. A. K., H. Rahimpour-Bonab, V. Tavakoli& M. Hosseindoost, 2009. Evidence for Late Holocene high-stands in Central Gilān–East Mazanderan, South Caspian coast, Iran. Quaternary International, 197: 55–71.
39. Lahijani, H: 1997. Riverine sediment and stability of the Iranian coast of the Caspian Sea.Russian Academy of Sciences. SCC.Caspy.120 p.
40. Lak, R., 1394. Sedimentation study of areas susceptible to the production of rapeseed in the marginal lands of the northwest of Lake Urmia, Geological Survey of Iran.206 p.
41. Leeder, M.R.; 1982.Sedimentology, processes and product. UNWIN HYMAN. 344.
42. Lee, Y., 1999- Geochemical characteristics of the Manhang Formation (Late Carboniferous) sandstones, Korea: implication for provenance. Geosciences Journal, v.3, 87-94.
43. Leontiev, O.K: 1977. Geomorphology of the Iranian coast of the Caspian Sea, Russian Academy of Sciences.
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Published
2020-04-10
How to Cite
Moghadam, B., Rezaei, K., Solgi, A., Ghiahchi, P., & Aleali, M. (2020). Gradation and geochemistry of the Fenced Lagoon sediments (Bandar Anzali) with regard to source rock and tectonic location. Journal of Geology, Geography and Geoecology, 29(1), 154-165. https://doi.org/https://doi.org/10.15421/112014
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