Génesis y evolución de las forma parakársticas de vallada a partir del estudio sedimentológico de sus rellenos
DOI:
https://doi.org/10.7203/CGUV..14990
Abstract
Se estudia la génesis y episodios evolutivos de un aparato kárstico desarrollado sobre materiales yesíferos en Vallada (Valencia), a partir de su estudio geomorfológico y análisis sedimentológicos. Esto permite diferenciar tres terrazas subterráneas y correlacionarlas con otros depósitos fluviales epigeos (río Cànyoles). Finalmente se establece una interpretación paleoclimática considerando datos polínicos y dos fechaciones radiocarbónicas.
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