Información del autor
Documentos disponibles escritos por este autor (4)
Añadir el resultado a su cesta Hacer una sugerencia Refinar búsqueda
texto impreso
Lloret, Joan ; Horra del Barco, Raúl de la ; Gretter, Nicola ; Borruel Abadía, Violeta ; Fernández Barrenechea, José María ; Ronchi, Ausonio ; Diez, José B. ; Arche, Alfredo ; López Gómez, José Trinidad | Elsevier | 2020-09This work focuses on the Olenekian-Anisian (Early-Middle Triassic) continental record of the Central-Eastern Pyrenean basin (NE Spain), a near-equator (10°-14°N) basin located in the western peri-Tethys margin, inside the Variscan fold-belt. Due[...]texto impreso
López Gómez, José ; Martín González, Fidel ; Heredia, N. ; Horra, Raúl de la ; Barrenechea, José F. ; Cadenas, Patricia ; Juncal, Manuel ; Diez, José B. ; Borruel-Abadía, Violeta ; David Pedreira, David ; García-Sansegundo, Joaquín ; Farias, Pedro ; Galé, Carlos ; Lago, Marceliano ; Ubide, Teresa ; Fernández-Viej, Gabriela ; Georges Gand, Georges | Elsevier | 2019-01The Pyrenean-Cantabrian Orogen arose through the collision of the Iberian and Eurasian plates, mostly in Cenozoic times. This orogen comprises two main mountain ranges, the Pyrenees to the east, and the Cantabrian Mountains to the west. To date,[...]texto impreso
Juncal Rosales, Manuel Antonio ; Lloret, Joan ; Diez, José B. ; López Gómez, José ; Horra, Raúl de la ; Barrenechea, José F. ; Arche, Alfredo | Elsevier | 2019-02In the western European basins, the paleoflora of late Pennsylvanian-early Permian transition is still a matter of discussion in terms of its age determination and biostratigraphic ranges. This study represents a review of the Upper Carboniferou[...]texto impreso
Juncal Rosales, Manuel Antonio ; Diez, José B. ; Horra del Barco, Raúl de la ; Galán Abellán, Ana Belén ; Borruel Abadía, Violeta ; Fernández Barrenechea, José María | Taylor & Francis | 2018The Triassic record in the SE Iberian Ranges starts with two tecto-sedimentary units of continental origin in Buntsandstein facies: and Cañizar and Eslida Formations. The Eslida Formation always lies conformably on top of the Cañizar Formation a[...]
