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The Meriadzek Terrace: A marginal plateau
Authors:S G Smith  E D Van Riessen
Institution:(1) Dept. of Geodesy and Geophysics, Cambridge, UK;(2) Vening Meinesz Laboratorium, Utrecht, The Netherlands;(3) Shell International Petroleum Company, The Hague, The Netherlands
Abstract:The Meriadzek Terrace forms part of the continental margin in the Bay of Biscay at a depth between that of the Continental shelf and the abyssal plain. Reflection profiles show that it is bounded on either side by basement ridges with a sediment infill between the ridges. It was probably formed by downfaulting of the continental shelf, possibly connected with the opening of the Bay of Biscay.
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