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Palygorskite in the recent fluvio-lacustrine and deltaic sediments of southern Mesopotamia

Published online by Cambridge University Press:  09 July 2018

A. A. M. Aqrawi
A. A. M. Aqrawi*
Affiliation:
Department of Geology, Royal School of Mines, Imperial College of Science, Technology and Medicine, Prince Consort Road, London SW7 2BP, UK
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Extract

Palygorskite has been widely reported as a clay phase in the Recent sediments of the northern Arabian Gulf (e.g. Aqrawi & Sadooni, 1988). It is usually thought to have originated from the sediments and soils of the Mesopotamian flood plains introduced by northwesterly (Shamal) winds (e.g. A1-Bakri et al., 1984). A1-Rawi et al. (1969) and Eswaran & Barzanji (1974) have detected palygorskite within Mesopotamian soils. This paper describes the occurrence of palygorskite in the Recent sediments of southern Mesopotamia and its possible origins will be discussed.

Type
Notes
Information
Clay Minerals , Volume 28 , Issue 1 , March 1993 , pp. 153 - 159
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1993

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References

Al-Bakri, D., Khalaf, F. & Al-Ghadban, A. (1984) Mineralogy, Genesis and sources of surficial sediments in the Kuwait marine-environment, Northern Arabian Gulf. J. Sed. Pet. 54, 1266–1279.Google Scholar
Al-RAWI, A.H., Jackson, M.L. & Hole, F.D. (1969) Mineralogy of some arid and semi-arid land soils of Iraq. Soil Sci. 107, 480–486.Google Scholar
Aqrawi, A.A.M. & Evans, G. (1990) Recent sediments of the lakes and marshes (Ahwar) of southern Mesopotamia. British Sedimentological Research Group (BSRG) Meeting, Reading, Abstracts. Google Scholar
Aqrawi, A.A.M. & Sadooni, F.N. (1988) Contribution of the eolian fall-out to the sediment budget in Khor A1-Zubair tidal flat, Nw Arabian Gulf, S. Iraq. Proc. Int. Sym. Geology Deserts Desert Environment, Unesco, Baghdad, l , 1-12.Google Scholar
Caillere, M.S. & Henin, S. (1951) Palygorskite-attapulgite. Pp. 234-243 in: X-ray Diffraction and Crystal Structure of Clay Minerals. Mineralogical Society, London.Google Scholar
Eswaran, J. & Barzanji, A.F. (1974) Evidence for the neoformation of attapulgite in some soils of Iraq. 10th Int. Congr. Soil Sci. Trans. Moscow, 7, 154–160.Google Scholar
Hudson, R.G.S., Eames, F.E. & Wilkins, G.L. (1957) The fauna of some Recent marine deposits near Basrah, Iraq. Geolog. Mag. 94, 393–401.CrossRefGoogle Scholar
Schultz, L.G. (1964) Quantitative interpretation of mineralogical composition from X-ray and chemical data for the Pierre Shale. U.S. Geol. Prof. Pap. 391-C. Google Scholar
Shaw, H.F. (1972) The preparation of oriented clay mineral speciments for X-ray diffraction analysis by a suctiononto-ceramic tile method. Clay Miner. 9, 349–350.Google Scholar
Singer, A. (1984) Pedogenic palygorskite in the arid environment. Pp. 169-175 in. Palygorskite-Sepiolite: Occurrence, Genesis and Uses (A. Singer & E. Galan, Editors). Developments in Sedimentology 37, Elsevier, Amsterdam.Google Scholar
Tanner, C.B. & Jackson, M.L. (1947) Monographs of sedimentation times for soil particles under gravity or centrifugal accelaration. Proc. Soil Sci. Soc. Am.12, 60-65.Google Scholar
Weaver, C.E. & Beck, K.C. (1977) Miocene of the S.E. United States: a model for chemical sedimentation in a perimarine environment. Sed. Geol. 17, 1–234.Google Scholar
White, S.H., Shaw, H.F. & Huggett, J.M. (1984) The use of backscattered electron imaging for the petrographic study of sandstones and shales. J. Sed. Pet. 54, 487–494.Google Scholar