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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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