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Eustatic movements generate intricate patterns of coastal units. The resulting stratigraphyc architecture depends on eustasy sediment supply and local tectonics. Tri-dimensional relatians due to sea-level changes are interesting because they all[...]texto impreso
Dabrio, Cristino J. ; Polo Camacho, María Dolores | Real Sociedad Española de Historia Natural | 1981El retrabajado marino del sedimento de las ramblas es el elemento básico del modelo dinámico del litoral del Puerto de Mazarrón. Los oleajes del segundo y del tercer cuadrantes producen, al incidir oblicuamente en la costa, corrientes de deriva [...]texto impreso
Dabrio, Cristino J. ; Borja, Francisco ; Zazo Cardeña , Caridad ; Boersma, Jan Richard ; Lario, Javier ; Goy Goy, José Luis ; Polo Camacho, María Dolores | Sociedad Geológica de España | 1996Facies analysis and tridimensional relationships of the eolian and eolian-connected deposits of Pleistocene and Holocene age in Huelva allow to proprose sedimentary models and discuss their temporal evolution and chronology.texto impreso
Dabrio, Cristino J. ; Polo Camacho, María Dolores | Granada : Secretariado de Publicaciones de la Universidad, C.S.I.C, Sección de Geología de la Facultad de Ciencias | 1972The study of the lower member materials of the Santiago de la Espada Formation reveals the existence of two different sedimentary environments, whose characteristics are analyzed in detail.texto impreso
Dabrio, Cristino J. ; Polo Camacho, María Dolores | Servicio de Publicaciones de la Universidad Complutense de Madrid | 1991Tortonian sedimentation in the Betics records a major tectonic event, the largest orogenic defonnation of the cordillera. superimposed on the largerscale, lhird-order TB 3.2 cyc1e of eustatic sea-level change. A first intetpretation of the Seque[...]texto impreso
During landward migration, ridge and runnel systems are subjected to asymmetric oscillatory and/or unidirectional flow regimes, depending on the stage of development reached by these systems. In the early stages of evolution, when the ridge is s[...]texto impreso
Dabrio, Cristino J. ; Fernández, Juan ; Polo Camacho, María Dolores | Granada : Secretariado de Publicaciones de la Universidad, C.S.I.C, Sección de Geología de la Facultad de Ciencias | 1971The authors define the Santiago de la Espada Formation and show its distinghishings characteristics. The limits and contacts as well as its observed shape and dimensions are described. The possible correlations with neighbouring sectors are poin[...]texto impreso
La fracturación hidráulica es una técnica conocida y utilizada industrialmente desde hace casi setenta años, pero en las dos últimas décadas ha experimentado un avance espectacular.Trata de explotar los denominados “hidrocarburos no convencional[...]texto impreso
Zazo Cardeña, Caridad ; Mercier, Norbert ; Silva Barroso, Pablo Gabriel ; Dabrio, Cristino J. ; Goy Goy, José Luis ; Roquero, Elvira ; Soler Javaloyes, Vicente ; Borja, Francisco ; Lario, Javier ; Polo Camacho, María Dolores ; Luque, Luis de | Elsevier Science B.V., Amsterdam | 2005The coastal evolution of the El Abalario area (Huelva, southern Spain) during the Late Pleistocene and Holocene is reinterpreted after a refinement of the available geochronology by means of optically stimulated luminescence (OSL) dating. New da[...]texto impreso
Roep, Th.B. ; Dabrio, Cristino J. ; Fortuin, A.R. ; Polo Camacho, María Dolores | Elsevier Science B.V. | 1998-02The late Messinian Sorbas Member, up to 75 m thick, consists in its type area of a parasequence sel of three prograding coastal barriers (sequences I-III), associated With lagoon and washover sediments. Around the town of Sorbas these strata can[...]texto impreso
Dabrio, Cristino J. ; Roep, Th.B. ; Polo Camacho, María Dolores ; Fortuin, A.R. | Sociedad Geológica de España | 1997Deposition of washover fans in coastal settings are related to accommodation space, slope of the basin margin, and coeval changes of sea level. Some preliminar y models of development and stacking of sand bodies are presented. [RESUMEN] El depós[...]texto impreso
Two models of reef growth are proposed for the Neogene reefs inlerbedded into the siliciclastic rocks af the narrow, fault-controlled Almanzora Basin: patch reefs on actively-prograding fan deltas (e.g. Purchena and Serón) and fringing reefs on [...]texto impreso
Zazo Cardeña , Caridad ; Dabrio, Cristino J. ; Borja, Francisco ; Goy Goy, José Luis ; Lezine, Anne Marie ; Lario Gómez, Javier ; Polo Camacho, María Dolores ; Hoyos Gómez, Manuel ; Boersma, J.R. | Royal Geological and Mining Society of the Netherland | 1999The stratigraphic relationships, genesis and chronology, including radiocarbon dating, of the Quaternary sandy deposits forming the El Asperillo cliffs (Huelva) were studied with special emphasis on the influence of neotectonic activity, sea-lev[...]texto impreso
Dabrio, Cristino J. ; Polo Camacho, María Dolores | Asociación Española para la Enseñanza de las Ciencias de la Tierra | 2005Los tsunamis, grandes olas extraordinarias típicamente asociadas a terremotos, inundan las zonas costeras provocando erosión y modificaciones morfológicas, pero también transporte y depósito de sedimento en las islas barrera, flechas, estuarios [...]
