Pilar Clariana
0000-0002-4168-2744
Universidad de Zaragoza
35 papers found
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Evolución Geodinámica de los Andes argentinochilenos y la Peńınsula Antártica durante el Neoproterozoico tard́ıo y el Paleozoico
Estratigrafía, estructura y su relación con el metamorfismo de la Zona Axial pirenaica en la transversal del Noroeste de Andorra y comarcas del Pallars Sobirá y el Alt Urgell (Lleida)
The Chanic structure of the San Rafael block (S Mendoza, Argentina): evidence of Chilenia – Cuyania collision
Metamorphic characteristics in the eastern part of the Pallaresa massif and their relationship with the variscan deformation events. Axial Zone of the Pyrenees (NW Andorra)
Clariana, P. & Garćıa-Sansegundo, J. (2012): Metamorphic characteristics in the Eastern part of the Pallaresa massif and their relationships with the variscan deformation events. Axial Zone of the Pyrenees (NW Andorra)
Hinterland-foreland zonation of the Variscan orogen in the Central Pyrenees: Comparison with the northern part of the Iberian Variscan Massif
Variscan structure in the eastern part of the Pallaresa massif, Axial Zone of the Pyrenees (NW Andorra). Tectonic implications
The structure in the Bagneres de Luchon and Andorra cross sections (Axial Zone of the central Pyrenees)
Estudi estratigràfic i estructural de la zona del parc natural de Sorteny
The structure in the Bagneres de Luchon and Andorra region cross-sections (Axial Zone of the central Pyrenees)
Presence of large north-verging folds in the Eastern sector of Pallaresa massif and the western sector of Hospitalet dome: main features and tectonic implications. Andorra, central Pyrenees.
Micro and mesostructural evidences of north-verging folds in the eastern sector of Pallaresa massif, Axial zone, central Pyrenees
Datos preliminares, estratigráficos y estructurales, obtenidos a partir de la cartografía del sinclinorio de Tor-Casamanya (Andorra, Pirineos Centrales)
Significado de los Pliegues N-S en el área del Río Civis. Sector Oriental del Flanco Sur del Sinclinal de Llavorsí. (Zona Axial, Pirineos Centrales)
Secuencia sedimentaria del Ordovícico Superior en el margen occidental del Domo del Orri (Pirineos Centrales)
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