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2009
DOI: 10.1680/cien.2009.162.6.18
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Engineering in the Barzaman formation, coastal Dubai, UAE

Abstract: This paper describes a geological model for the ‘conglomeratic carbonate siltstone’, otherwise known as the Barzaman formation, which comprises the principal founding stratum for deep structures in coastal Dubai, UAE. It identifies and highlights some important considerations for future engineering works in this stratum. A brief review of the geology and geotechnical characteristics of the stratum is provided, followed by a discussion of recent work on those aspects of the mineralogy and geotechnical propertie… Show more

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Cited by 6 publications
(2 citation statements)
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“…The country is generally relatively low-lying, with the exception of the mountainous regions within the northeast of the country, dominated mainly by deposits of Quaternary to late Pleistocene age, including mobile Aeolian dune sands, evaporate deposits, and marine sands (Cherian 2018). Dubai is situated towards the eastern border of the geologically stable Arabian Plate due to the presence of rocks and separated from the unstable Iranian Fold Belt to the north by the Arabian Gulf (Macklin and Gaba 2009). The ground conditions comprise the horizontally stratified subsurface profile which was complex and highly variable, because of the character of deposition and also the prevalent hot arid weather conditions.…”
Section: Geology and Subsurface Conditionsmentioning
confidence: 99%
“…The country is generally relatively low-lying, with the exception of the mountainous regions within the northeast of the country, dominated mainly by deposits of Quaternary to late Pleistocene age, including mobile Aeolian dune sands, evaporate deposits, and marine sands (Cherian 2018). Dubai is situated towards the eastern border of the geologically stable Arabian Plate due to the presence of rocks and separated from the unstable Iranian Fold Belt to the north by the Arabian Gulf (Macklin and Gaba 2009). The ground conditions comprise the horizontally stratified subsurface profile which was complex and highly variable, because of the character of deposition and also the prevalent hot arid weather conditions.…”
Section: Geology and Subsurface Conditionsmentioning
confidence: 99%
“…These rocks laid down in a various deposition, principally shallow marine, intertidal, fluvial environments and sabkha [31]. These rocks have also been affected by relatively limited deformations associated with the anti-clockwise ongoing movement of the Arabian plate towards the Eurasian plate [32,33].…”
Section: Regional Geological Settingmentioning
confidence: 99%