Monique Mettraux

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The Bar Al Hikman peninsula located on the eastern coast of Oman has developed over the Pleistocene and Holocene as an in situ shallow water carbonate/evaporite system with subordinate amounts of clastic sand and gravel. In this study different resolutions of satellite imagery ranging from low, medium to high and acquired between 1972 and 2004, were used to(More)
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