Canales arenosos de la Formación Nájera: Características Deposicionales y factores de control
Sandy Channels of the Nájera Formation: Depositional Characteristics and control factors
dc.contributor.author | Molinero Huguet, J. | |
dc.contributor.author | Colombo Piñol, Ferrán | |
dc.date.accessioned | 2016-04-08T10:45:44Z | |
dc.date.available | 2016-04-08T10:45:44Z | |
dc.date.issued | 1996 | |
dc.identifier.uri | http://hdl.handle.net/10272/11822 | |
dc.description.abstract | The studied sedimentological section is located in continental tertiary sediments of the western part of the Ebro Basin, and have been interpreted as being generated by braided streams in a general depositional subenvironment corresponding to the external zones of alluvial fans. In this context we found channel deposits with characteristics that are typical of meandering rivers, suggesting that some streams with a sinuous thalweg circulated within this braid plain. The significant agradational pattern shown by these deposits was conditioned by both the lithological characteristics of the bed and the extra sedimentary supply from a local relief which was formed in response to the activity of a blind thrust | en_US |
dc.language.iso | spa | en_US |
dc.publisher | Sociedad Geológica de España | en_US |
dc.rights | Atribución-NoComercial-SinDerivadas 3.0 España | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/es/ | * |
dc.subject.other | Channels | en_US |
dc.subject.other | Tectonics | en_US |
dc.subject.other | Sedimentation | en_US |
dc.subject.other | Najera Formation | en_US |
dc.subject.other | Ebro Basin | en_US |
dc.subject.other | La Rioja | en_US |
dc.title | Canales arenosos de la Formación Nájera: Características Deposicionales y factores de control | en_US |
dc.title | Sandy Channels of the Nájera Formation: Depositional Characteristics and control factors | eng |
dc.type | info:eu-repo/semantics/article | en_US |
dc.rights.accessRights | info:eu-repo/semantics/openAccess | en_US |