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Browsing by Author "Robador, Alejandro"
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Una importante discontinuidad estratigráfica del Paleoceno de Navarra y del País Vasco: caracterización y significado
Robador, Alejandro; Pujalte, Victoriano; Orue Etxebarria, Xabier; Baceta, Juan Ignacio; Robles, Santiago (Sociedad Geológica de España, 1990)An important stratigraphic break has been recognized in the Paleocene of Navarra and the Basque Country, which is recorded with different features, both in platform and basinal settings. lt has been correlated through ... -
La Fm Puerto de La Losa (N de Granada, E de Jaén): una nueva unidad estratigráfica, paleogeográficamente significativa, del Paleógeno Inferior Prebético
Pujalte, Victoriano; Orue Etxebarria, Xabier; Apellaniz, Estíbali; Baceta, Juan Ignacio; Payros, Aitor; Robador, Alejandro; Tosquella Angrill, Josep(2010)
A new unit has been recognized in the Prebetic of the northern part of the Granada Province and eastern part of the Jaén Province, herein defined as La Losa Pass Fm and dated with planktonic and larger foraminifera as late ... -
Un mapa geológico inédito de Ceuta de Máximo Laguna y Luis Satorras (1861)
Boixereu Vila, Ester; Robador, Alejandro (Sociedad Geológica de España, 2021)En la biblioteca del Ministerio de Defensa se conserva un ejemplar de un mapa manuscrito titulado “Croquis geológico de Montes de Sierra Bullones a escala 1:20.000”, firmado por los ingenieros de montes Máximo Laguna y ... -
Redefinition of the Ilerdian Stage (early Eocene)
Pujalte, Victoriano; Baceta, Juan Ignacio; Schmitz, B.; Orue Etxebarria, Xabier; Payros, Aitor; Bernaola, Gilen; Apellaniz, Estíbali; Caballero, F.; Robador, Alejandro; Serra Kiel, Josep; Tosquella Angrill, Josep(Consejo Superior de Investigaciones Científicas; Universidad de Barcelona; Universidad Autónoma de Barcelona, 2009)
The Ilerdian Stage was created by Hottinger and Schaub in 1960 to accommodate a significant phase in the evo¬lution of larger foraminifera not recorded in the northern European basins, and has since been adopted by most ... -
Registro geológico del máximo térmico del Paleoceno-Eoceno en el Parque Nacional de Ordesa y Monte Perdido (Pirineo Central)
The Paleocene-Eocene thermal maximun (PETM) had earlier been documented in basinal and continental settings of the Pyrenean basin clastic units. In this work new data are added from comparatively less well-known platform ...