The study of the present granolumetric facies plot of surficial sediment sample and high resolution seismic profile analysis, allow us to establishment the general aspects of the Holocene sediment dynam ic evolution in the Northern Continental shelf of Cádiz Gulf. The relationship betwen diferent facies has been considerated in relation to the mean eustatic events and oceanografic condition enforce by the dynamic ofNorAtlantic Surficial Water (NASW) on the shelf
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