Información del autor
Documentos disponibles escritos por este autor (3)
Añadir el resultado a su cesta Hacer una sugerencia Refinar búsqueda
texto impreso
The Feos Formation of the Nijar Basin comprises sediments deposited during the final stage of the Messinian salinity crisis when the Mediterranean was almost totally isolated. Levels of soft-sediment deformation structures occur in both conglome[...]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[...]
