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The geological record of the oldest historical tsunamis in southwestern Spain
(Università degli Studi di Milano, 2008-03)
A regressive sequence was determined in the late Ho- locene evolution of the southwestern Donana National Park (SW Spain), based on a multidisciplinary study of sediments obtained in a drill core. In an initial phase (> ...
Reply to the comment by A. Rodríguez Ramírez on “The geological record of the oldest historical tsunamis in southwestern Spain” by Francisco Ruiz, Manuel Abad, Joaquín Rodríguez-Vidal, María Isabel Carretero, Manuel Pozo & Francisco Gómez Toscano, published in Rivista Italiana di Paleontologia e Stratigrafia, 114(1): 147-156 (2008)
(Università degli Studi di Milano, 2009-03)
Análisis y cartografía de riesgos geológicos en el litoral de la ciudad autónoma de Ceuta
(Universidad de Huelva, 2009)
Rasgos morfológicos y bioerosivos en un alto nivel marino del pleistoceno medio : el abrigo arqueológico de la Cabililla de Benzú (Ceuta)Morphologic and bioerosive features from an old marine highstand: the Cabililla archaeological shelter, Benzú, Ceuta
(Asociación Española para el Estudio del Cuaternario, 2007)
The micro-morphologic and bioerosive features, analyzed in the Benzú shelter (Ceuta), allow us to deduce an erosion
marine surface elaborated onto dolomite triassic substrate. The Entobia-Gastrochaenolites Ichnoassociation ...
Rasgos morfológicos y bioerosivos en un alto nivel marino del pleistoceno medio : el abrigo arqueológico de la Cabililla, Benzú, Ceuta
(Asociación Española para el Estudio del Cuaternario, 2007)
El Control del Paleorrelieve durante la Transgresión Tortoniense: Un Caso de Estudio en el Margen Pasivo de la Cuenca del Guadalquivir (Sur de España)The Effect of Paleotopography on the Tortonian Transgresion: A case study in the Guadalquivir Foreland Basin (South Spain)
(Sociedad Geológica de España, 2005)
The Guadalquivir foreland basin has a complex temporal and spatial evolution which is shown in its facies
architecture and its paleogeographical distribution during Tortonian. In this work we emphasize the control
that ...
Génesis y caracterización del cordón estuarino de Las Nuevas (P. N. de Doñana)Origin and characterization of the estuaríne ridge of Las Nuevas (Doñana National Park)
(Sociedad Geológica de España, 2000)
The georñorphological and palaeontological studies of the Las Nuevas estuaríne ridge indicates that these silty sands with abundant macrofaune were deposited over clayey marsh deposits during some erosive events at ...
Respuesta Estratigráfica a la Transgresión Tortoniense en el Margen Pasivo de la Cuenca del Guadalquivir: Datos PreliminaresStratigraphical response to the Tortonian Transgression in the Guadalquivir Foreland Margin: A preliminary approach
(Sociedad Geológica de España, 2005)
The passive margin of the Guadalquivir foreland basin records different stages of evolution during the
tortonian transgression, mainly determinate by sedimentary supply/ accommodation space ratio (A/S ratio,
Cattaneo and ...
Morphosedimentary evidence of the Last Interglacial Maximum on the coast of Governor’s Beach, GibraltarEvidencias morfosedimentarias del Último Máximo Interglacial en la costa de Governor’s Beach, Gibraltar
(2007)
Los registros marinos, erosivo-sedimentarios, en la costa de Gibraltar son el resultado de episodios de
elevaciones eustáticas, sobre los que se depositan secuencias continentales eólicas y gravitacionales de
descenso ...
Análisis de modelados de erosión y depósitos residuales transgresivos en el Sector Central de la Cuenca del Guadalquivir (Tortoniense, SO de España)Analysis of erosive modelated and transgressive lag deposits in the Central Sector of the Guadalquivir Basin (Tortonian, SW Spain)
(Sociedad Geológica de España, 2004)
The central sector of the northern foreland margin of the Guadalquivir Basin shows good examples of
transgressive erosion surfaces, recognisable along all its extension. In the studied area (Villanueva del Rio y
Minas, ...