Facies architecture and origin of the Quaternary sand dunes of the Qazvin Plain, Iran

Document Type : Research Paper

Authors

1 Department of Geology, Faculty of Sciences, Bu-Ali Sina University, Hamedan, Iran

2 Department of Geography, Faculty of Sciences, Imam Ali University, Tehran, Iran

Abstract

Sand dunes of the Quaternary age occupy large areas of Iran’s semiarid and arid regions. In this study, some 33 sediment samples were collected from the crest, the lee and stoss sides of the linear dunes of the southern part of Qazvin plain. Sedimentological, geochemical, and mineralogical investigations were carried out in order to identify the origin and probable source of the aeolian dune sands. Grain size analysis of the sediments shows that most of the aeolian sands are generally fine-grained, moderately well-sorted, fine skewed and leptokurtic. The textural, mineralogical and the geochemical results supported by the statistical approach indicate that the dune sands were mainly derived from the Quaternary flood plain with a minor contribution from alluvial and fluvial sands. Facies study leads to the determination of 4 facies in 2 facies associations, including: 1) medium-grained lithofacies (Sdpc, Sdl, and Sdm), and 2) gypcrete facies (G). The studied aeolian sands are characterized by the predominance of gypsum and quartz, and stable minerals together with sedimentary, metamorphic, and volcanic fragments, and a few unstable pyroxene and amphibole minerals. The sand dunes of the Qazvin Plain record a semi-arid to arid paleoclimate and the relatively stable tectonic background characterized by the mineralogical and geochemical composition and gypcrete facies in the dunes.

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Main Subjects

Article Title [Persian]

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References

Aljubouri, Z. A., 2011. Geochemistry of calcium sulphate rocks of Fatha Formation at four localities within Nineveh District, Northern Iraq (with emphasis on strontium distribution). Iraqi National Journal of Earth Sciences 11: 49-70.
Alles, D. L., 2013. China's desert. Western Washington University, Washington, USA, 52 pp.
Alonso-Zarza, A.M., 2003. Palaeoenvironmental significance of palustrine carbonates and calcretes in the geological record. Earth Science, 60: 261 -298.
Alonso-Zarza, A.M., 2018. Study of a modern calcrete forming in Guadalajara, Central Spain: An analogue for ancient root calcretes. Sedimentary Geology, 373: 180-190.
Annells, R.N., Arthurton, R.S., Bazley, R.A., Davies, R.G., 1975. Explanatory text of the Qazvin and Rasht quadrangles map. 1:250.000. Geological Survey of Iran. Geological Quadrangles Nos. E3-E4. In Persian.
Bagnold, R. A. 1941. The Physics of Blown Sand and Desert Dunes London, Methuen. 265 pp.
Berberian, M., Qorashi, M., Arzhang-ravesh, B., Mohajer-Ashjai, A., 1993. Recent tectonics, seismotectonics and
earthquake-fault hazard investigation in the Greater Qazvin region:contribution to the seismotectonics of Iran. Geology Survey of Iran, 197 pp.
Besler, H., 2008. The Great Sand Sea in Egypt. Developments in Sedimentology, 59. Elsevier., Amsterdam, 250 pp.
Bingqi, Z., Jingjie, Y., 2013. Aeolian sorting processes in the Ejina desert basin China) and their response to depositional environment. Aeolian Research, 12: 111- 20.
Busacca, A.J., Beget, J.E., Markewich, H.W., Muhs, D.R., Lancaster, N., Sweeney, M.R., 2003. Eolian sediments. In: Gillespie, A.R., Porter, S.C., Atwater, B.F. (Eds.), De- velopments velopments in Quaternary Sciences. Elsevier, pp. 275-309.
Carver, R.E., 1971. Procedures in Sedimentary Petrology, Wiley Interscience, New York. pp. 49-69.
Clyde, W.C., Ting, S.Y., Snell, K.E., Bowen, G.J., Tong, Y.S., Koch, P.L., Li, Q., Wang, Y.Q., 2010. New Paleomagnetic and Stable-Isotope Results from the Nanxiong Basin, China: Implications for the K/T Boundary and the Timing of Paleocene Mammalian Turnover. Journal of Geology, 118: 131-143.
Davoudi, V., Khodabakhsh, S., Rafiei, B., 2019. Alluvial fan facies of the Qazvin Plain: paleoclimate and tectonic implications during Quaternary. Geopersia, 10 (1): 65-87
Dickinson, W.R., 1970. Interpreting detrital modes of greywacke and arkose. Journal of Sedimentary Petrology, 40: 695-707.
Fitzsimmons, K.E., 2007, Morphologic Variability in the Linear Dune Fields of the Strzelecki and Tirari Deserts, Australia. Geomorphology, 91: 146-160.
Folk, E., 1980. Petrography of Sedimentary Rocks. Hemphill Publishing Company. 182 pp.
Gazzi, P., 1966. Le arenarie Del flysch sopracretaceo deU’Appennmo modenese; correlazioni conil flysch di Monghidoro. In: Dickinson, W.R., Beard L.S., Brakenridge, G.R., Erjavec J.L., Ferguson, R.C. and Inman K.P. 1983a.Provenance of North American Phanerozoic sandstones in relation to tectonic setting. Geological Society of America Bulletin, 94: 22-35.
Ghinassi, M., Ielpi, A., 2016. Morphodynamics and facies architecture of stream flow-dominated, sandrich alluvial fans, Pleistocene Upper Valdarno Basin, Italy. In: Ventra, D. & Clarke, L.E. (eds) Geology and Geomorphology of Alluvial and Fluvial Fans: Terrestrial and Planetary Perspectives. Geological Society, London, Special Publications, 440 pp.
Gough, A. 2015. Controls on sediment architecture and deposition in arid continental basin margin systems, this thesis is submitted for the degree of Doctor of Philosophy of the University of Keele, 505 pp.
Hunter, R.E., 1977. Terminology of cross-stratified sedimentary layers and climbing-ripple structures. Sedimentary Research, 47 (2): 697-706
Kasper-Zubillaga, J.J., Carranza-Edwards, A., 2005. Grain size discrimination between sands of desert and coastal dunes from northwestern Mexico. Revista Revista Mexicana de Ciencias Geológicas, 22 (3): 383-390.
Kocurek, G., Havholm, K.G., 1993. Eolian sequence stratigraphy - a conceptual framework. In: Weimer, P., Posamentier, H.W. (Eds.), Siliciclastic sequence stratigraphy: recent developments and applications. Society of Economic Paleontologists and Mineralogists, Special Publication, 52: 393-409.
Kocurek, G.A., 1991. Interpretation of ancient eolian sand dunes. Annu. Rev. Earth Planet. Planet Science, 19: 43-75.
Lancaster, N., 1981. Grain size characteristics of Namib Desert linear dunes: Sedimentology, 28: 115-122.
Lancaster, N., 1986. Grain-size characteristics of linear dunes in the southwestern Kalahari, Sedimentary Petrology, 56 (3): 395-400.
Livingstone, I., 1989. Temporal trends in grain-size measures on a linear sand dune. Sedimentary Research, 6: 1017-1022.
Livingstone, I., Bullard, J.E., Wiggs, G.F.S., Thomas, D.S.G., 1999. Grain-size variation on dunes in the southwest Kalahari, Southern Africa, Sedimentary Research, 69: 546-552.
Madole, R. F., Romig, J. H., Aleinikoff, J. N., VanSistine, D. and Yacob, E., 2008. On the origin and age of the great sand dunes, Colorado. Geomorphology, 99: 99-119.
Mangimeli, J., 2007. White Sands National Monument. Geology of Sand Dunes. 2-11 pp.
MCKEE, E.D., 1966. Structures of dunes at White Sands National Monument, New Mexico (and a comparison with structures of dunes from other selected areas). Sedimentology, 7: 1-69.
Miall, A.D., 2006. The Geology of Fluvial Deposits: Sedimentary Facies, Basin Analysis, and Petroleum Geology, Springer, 582 pp.
Mountney, N.P., 2006. Eolian Facies Models. In: Walker, R.G., Posamentier, H.W. (Eds.), Facies
Models Revisited. SEPM Special Publication 84, Society for Sedimentary Geology, Oklahoma, pp. 19-83.
Muhs, D.R., 2004. Mineralogical maturity in dune fields of North America, Africa and Australia. Australia. Geomorphology, 59: 247-269.
Muhs, D.R., Wolfe, S.A., 1999. Sand dunes of the northern Great Plains of Canada and the United States. In: Lemmen, D.S., Vance, R.E. (Eds.), Holocene Climate and Environmental Change in the Palliser Triangle: a Geoscientific Context for Evaluating the Effects of Climate Change on the Southern Canadian Prairies. Geological Survey of Canada, Ottawa, pp. 183-197.
Pavelic, D. Kovacic, M., Vlahovic, I., Wacha, L. 2011. Pleistocene calcareous aeolian-alluvial deposition in a steep relief karstic coastal belt (island of Hvar, eastern Adriatic, Croatia). Sedimentary Geology, 239: 64-79.
Pavelic, D., Kovacic, M., Vlahovic, I., 2006. Periglacial aeolian-alluvial interaction: Pleistocene of the Island of Hvar (Eastern Adriatic, Croatia). In: Hoyanagi, K., Takano, O., Kano, K. (Eds.), From the Highest to the Deepest: Abstracts, Volume A, 218 pp.
Reeves, C.C., 1983. Pliocene channel calcrete and suspenparallel drainage in West Texas and New Mexico. In: Wilson, R.C.L. (Eds.), Residual Deposits: Surface Related Weathering Processes and Materials. Geological Society of London Special Publication. Geological Society of London, 11:179-183.
Rezazadeh Balgori, B. 2016. Sedimentology and geochemistry of aeolian sand dunes in north of Ahangran (Zirkoh city, east of Iran). University of Birjand. 163 pp.
Rieben, E.H., 1966. Geological observations on alluvial depositions in northern Iran. Geological Survey of Iran, 39 pp.
Tsoar, H. 1978. The dynamics of longitudinal dunes. Final technical report. European Research Office, US Army. 76- -972 pp.
Tsoar, H. 1983. Dynamic Processes Acting On a Longitudinal (Seif) Dune. Sedimentology, 30: 567-578.
Visher, G. S., 1999, Grain size distributions and depositional processes: Journal of Sedimentary Petrology, 39: 1074-1106.
Wahby, W.S., 2004. Technologies Applied in the Toshka Project of Egypt. Journal of Technology Studies, 30: 86-91.
Wang, X.M., Dong, Z.B., Zhang, J.W., Qu, J.J., Zhao, A.G., 2003, Grain size characteristics of dune sand in the central Taklimakan Sand Sea: Sedimentary Geology, 16: 1-14.
Watson, A. 1985. The control of windblown sand and moving dunes: a review of the methods of sand control in deserts, with observations from Saudi Arabia. Quarterly Journal of Engineering Geology, 18: 237-52.
Watson, A., 1986. Grain-size variations on a longitudinal dune and a barchan dune: Sedimentary Geology, 46: 49-66.
Wright, V.P., Tucker, M.E., 1991. Calcretes. An introduction. In: Wright, V.P., Tucker, M.E. (Eds.), Calcretes. IAS Reprint Series. Blackwell, Oxford, 2: 1-22.

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History

  • Receive Date: 18 January 2023
  • Revise Date: 20 February 2023
  • Accept Date: 25 February 2023

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