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Zazo Cardeña, Caridad ; Dabrio, Cristino J. ; Goy Goy, José Luis ; Bardají Azcárate, Teresa ; Ghaleb, B. ; Lario, Javier ; Hoyos, M. ; Hillaire-Marcel, Claude ; Sierro, Francisco Javier ; Flores, José-Abel ; Silva Barroso, Pablo Gabriel ; Borja, Francisco | Sociedad Geológica de España | 1996The interaction between global factors ("global" glacio-eustatic sea-level rise) and regional factors (tectonic trend, oceanographic factor) is analyzed in different areas of the Iberian and Canary Island littoral. Sea-level changes and c1imatic[...]texto impreso
Lario, Javier ; Zazo Cardeña, Caridad ; Goy Goy, José Luis ; Dabrio, Cristino J. ; Borja, Francisco ; Silva Barroso, Pablo Gabriel ; Sierro, Francisco Javier ; González, A. ; Soler Javaloyes, Vicente ; Yll, E.I. | Elsevier | 2002An analysis of sedimentation rates during the Holocene in estuaries in the southwestern coast of the Iberian Peninsula using depth/age diagrams reveals the existence of two distinct phases. The first, between ca. 10,000 and 6500 Cal BP, still in[...]texto impreso
Dabrio, Cristino J. ; Zazo Cardeña , Caridad ; Goy Goy, José Luis ; Sierro, Francisco Javier ; Borja, Francisco ; Lario, Javier ; González Delgado, José Ángel ; Flores Villarejo, José Abel | Elsevier Science B.V., Amsterdam. | 2000The Late Pleistocene and Holocene evolution of the estuaries in the Gulf of Cadiz is interpreted for the first time using drill cores, logs, trenches, and 38 new radiocarbon data, and the results compared with the shelf. The Odiel, Tinto and Gua[...]texto impreso
Goy Goy, José Luis ; Zazo Cardeña , Caridad ; Dabrio, Cristino J. ; Lario, Javier ; Borja, Francisco ; Sierro, Francisco Javier ; Flores, José-Abel | Elsevier | 1996The interaction between global (glacio-eustatic sea-level rise) and regional factors (oceanographic and tectonic) has controlled the evolution of coastline during the Holocene in Southem Iberia. At ca. 10,000 14C years BP a deceleration of relat[...]texto impreso
Lario, Javier ; Zazo Cardeña , Caridad ; Plater, A.J. ; Goy Goy, José Luis ; Dabrio, Cristino J. ; Borja, Francisco ; Sierro, Francisco Javier ; Luque, Luis de | E. Schweizerbart'sche Verlagsbuchhandlung | 2002High resolution particle size and environmental magnetie analyses were earried out on two eores from marsh sediments in the Doñana National Park (SW Spain), in an investigation of gradual and abrupt eoastal change. Complementary palaeontological[...]texto impreso
Yll, R. ; Zazo Cardeña , Caridad ; Goy Goy, José Luis ; Perez Obiol, R. ; Pantaleón Cano, J. ; Civis Llovera, Jorge ; Dabrio, Cristino J. ; González , A. ; Borja, Francisco ; Soler Javaloyes, Vicente ; Lario, Javier ; Luque, Luis de ; Sierro, Francisco Javier ; González Hernández, F.M. ; Lezine, Anne Marie ; Denefle, Michael ; Roure, Joan Maria | Universidad de Alcalá | 2003This paper presents the existing differences between the evolution of the Holocene landscape of the Southeastern and Southwestern areas of the Iberian Peninsula. Moreover, some palaeoenvironmental characteristics of OIS 4 and OIS 3 of the wester[...]texto impreso
Dabrio, Cristino J. ; Zazo Cardeña , Caridad ; Lario Gómez, Javier ; Goy Goy, José Luis ; Sierro, Francisco Javier ; Borja, Francisco ; González Delgado, José Ángel ; Flores Villarejo, José Abel | Royal Geological and Mining Society of the Netherland | 1999This first sedimentary interpretation of two incised-valley fills in the Gulf of Cádiz (southern Spain), which accumulated during the last fourth-order eustatic cycle in response to fluvial incision, changes of sea level, and correlative deposit[...]texto impreso
Zazo Cardeña , Caridad ; Dabrio, Cristino J. ; González, A. ; Sierro, Francisco Javier ; Yll, E.I. ; Goy Goy, José Luis ; Luque, Luis de ; Pantaleón Cano, J. ; Soler Javaloyes, Vicente ; Roure, J.M. ; Lario, Javier ; Hoyos, M. ; Borja, Francisco | Sociedad Geológica de España | 1999El estudio de un sondeo de 65 m en las marismas del Guadalquivir permite reconocer siete intervalos que reflejan cambios climáticos y eustáticos e intensa neotectónica durante tres periodos interglaciares (IS 7?, 5 Y 1) Y dos glaciares (15 6-Ris[...]
