Significado sedimentológico de los niveles con Assilinas de la Formación Armancies (Eoceno medio) y sus equivalentes laterales

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Show simple item record Obrador Tuduri, Antoni Pallí i Buxó, Lluís Rosell Sanuy, Joan 1973
dc.identifier.issn 0567-7505
dc.description.abstract In this paper we show some sedimentological characteristics of Assilina beds from Armancies Fm. (middle Eocene) and their lateral equivalents that let us to remark some aspects of their genesis. We arrive to the conclusion that, in occidental sector (Bagá-Campdevanol), ‘las barras de Assilinas’ from the Armancies Fm. are grain flow channels, first sedimented at W of Terrades and after slided, from E to W in a turbidite basin, without any coarse clastic
dc.description.abstract En esta nota exponemos las características sedimentológicas de los niveles con Assilina de la Fm. Armancies y sus equivalentes laterales que permiten precisar algunos aspectos acerca de su génesis. Se llega a la conclusión de que las ‘barras de Assilinas’ de la Fm. Armancies, en su extremo occidental (Bagá-Campdevanol), son canales depositados originariamente al W de Terrades y deslizados, de E a W, en una cuenca turbidítica sin aportes de clásticos groseros
dc.format.mimetype application/pdf
dc.language.iso spa
dc.publisher Institut de Ciències de la Terra Jaume Almera
dc.relation.isformatof Reproducció digital del document publicat a:
dc.relation.ispartof © Acta geológica hispánica, 1973, vol. 8, núm. 1, p. 11-12
dc.relation.ispartofseries Articles publicats (D-CCAA)
dc.rights Tots els drets reservats
dc.subject Estratigrafia -- Eocè
dc.subject Sediments (Geologia)
dc.subject Geology, Stratigraphic -- Eocene
dc.subject Sediments (Geology)
dc.title Significado sedimentológico de los niveles con Assilinas de la Formación Armancies (Eoceno medio) y sus equivalentes laterales
dc.type info:eu-repo/semantics/article
dc.type.version info:eu-repo/semantics/publishedVersion

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