Irene Gómez Pérez, Pedro Angel Fernández Mendiola, Joaquín García Mondéjar
The Itxina carbonate platform displays a western reef-rimmed margin. Clinoforms up to 30-35 0 link this sha/low rim and basinal marls. Slope constructiona/ dynamics has been analyzed. Highstand slope progradation (offlap) alternates with Iowstand phases of destruction causing erosion and megabreccia formation
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