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   1. < dc:title > Abrasion processes in coarse-clastic beaches linked to rocky shore platforms </ dc:title >

   2. < dc:creator > Blanco Chao, Ramón </ dc:creator >

   3. < dc:creator > Pérez Alberti, Augusto </ dc:creator >

   4. < dc:creator > Costa-Casais, Manuela </ dc:creator >

   5. < dc:creator > Valcárcel Díaz, M. </ dc:creator >

   6. < dc:subject > Abrasión </ dc:subject >

   7. < dc:subject > Abrasion </ dc:subject >

   8. < dc:subject > Playas de material grueso </ dc:subject >

   9. < dc:subject > Coarse-grained beaches </ dc:subject >

   10. < dc:subject > Plataformas litorales </ dc:subject >

   11. < dc:subject > Shore platforms </ dc:subject >

   12. < dc:subject > Depósitos sedimentarios </ dc:subject >

   13. < dc:subject > Sedimentary deposits </ dc:subject >

   14. < dc:subject > NO España </ dc:subject >

   15. < dc:subject > NW Spain </ dc:subject >

   16. < dc:subject > Laboratorio de Patrimonio </ dc:subject >

   17. < dc:subject > Heritage Laboratory </ dc:subject >

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   24. < dc:description > [ES] La abrasión es uno de los procesos menos conocidos que operan en las costas rocosas. Este trabajo trata de mostrar algunos de los mecanismos básicos en este tipo de procesos, principalmente en playas de material grueso. Los dos factores principales en los procesos abrasivos son el balance de la energía de las olas y el tamaño del clasto, pero en áreas en las que la existencia de depósitos continentales fluvio-nivales y periglaciares son comunes, otros factores que funciona a escalas de tiempo media son también muy importantes. La morfología de las plataformas rocosas litorales y la erosión Holocena de los acantilados, formados por depósitos heterométricos desarrollados durante a última regresión marina, están fuertemente relacionados. </ dc:description >

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   2. < creator > Blanco Chao, Ramón </ creator >

   3. < creator > Pérez Alberti, Augusto </ creator >

   4. < creator > Costa-Casais, Manuela </ creator >

   5. < creator > Valcárcel Díaz, M. </ creator >

   6. < subject > Abrasión </ subject >

   7. < subject > Abrasion </ subject >

   8. < subject > Playas de material grueso </ subject >

   9. < subject > Coarse-grained beaches </ subject >

   10. < subject > Plataformas litorales </ subject >

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   24. < description > [ES] La abrasión es uno de los procesos menos conocidos que operan en las costas rocosas. Este trabajo trata de mostrar algunos de los mecanismos básicos en este tipo de procesos, principalmente en playas de material grueso. Los dos factores principales en los procesos abrasivos son el balance de la energía de las olas y el tamaño del clasto, pero en áreas en las que la existencia de depósitos continentales fluvio-nivales y periglaciares son comunes, otros factores que funciona a escalas de tiempo media son también muy importantes. La morfología de las plataformas rocosas litorales y la erosión Holocena de los acantilados, formados por depósitos heterométricos desarrollados durante a última regresión marina, están fuertemente relacionados. </ description >

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   3. < mods:name >

      1. < mods:namePart > Costa-Casais, Manuela </ mods:namePart >

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   4. < mods:name >

      1. < mods:namePart > Valcárcel Díaz, M. </ mods:namePart >

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   11. < mods:abstract > [ES] La abrasión es uno de los procesos menos conocidos que operan en las costas rocosas. Este trabajo trata de mostrar algunos de los mecanismos básicos en este tipo de procesos, principalmente en playas de material grueso. Los dos factores principales en los procesos abrasivos son el balance de la energía de las olas y el tamaño del clasto, pero en áreas en las que la existencia de depósitos continentales fluvio-nivales y periglaciares son comunes, otros factores que funciona a escalas de tiempo media son también muy importantes. La morfología de las plataformas rocosas litorales y la erosión Holocena de los acantilados, formados por depósitos heterométricos desarrollados durante a última regresión marina, están fuertemente relacionados. </ mods:abstract >

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   1. < dc:title > Abrasion processes in coarse-clastic beaches linked to rocky shore platforms </ dc:title >

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   4. < dc:subject > Playas de material grueso </ dc:subject >

   5. < dc:subject > Coarse-grained beaches </ dc:subject >

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   20. < dcterms:abstract > [ES] La abrasión es uno de los procesos menos conocidos que operan en las costas rocosas. Este trabajo trata de mostrar algunos de los mecanismos básicos en este tipo de procesos, principalmente en playas de material grueso. Los dos factores principales en los procesos abrasivos son el balance de la energía de las olas y el tamaño del clasto, pero en áreas en las que la existencia de depósitos continentales fluvio-nivales y periglaciares son comunes, otros factores que funciona a escalas de tiempo media son también muy importantes. La morfología de las plataformas rocosas litorales y la erosión Holocena de los acantilados, formados por depósitos heterométricos desarrollados durante a última regresión marina, están fuertemente relacionados. </ dcterms:abstract >

   21. < dcterms:abstract > [EN] Abrasion is one of the less known processes operating on rocky beaches. This work tries to show some of the basic mechanisms in this type of processes, namely in coarse-grained beaches. The two main factors in the abrasive processes are the balance wave energy and clast size, but in areas in which the existence of thick periglacial and fluvio nival continental deposits are common, other factors operating at medium time scales are also very important. The morphology of the rocky platforms and the Holocene erosion of cliffs shaped on heterometric deposits developed during the last marine regression, are strongly related. </ dcterms:abstract >

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      2. < field name =" mail " > julio.pemau@bib.csic.es </ field >

      </ element >

   5. < element name =" license " >

      1. < field name =" bin " > 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 </ field >

      </ element >

   </ metadata >