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Browsing by Author "Marzo, M."
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Diferentes estilos de organización secuencia! en depósitos de abanico aluvial y abanico costero lateralmente relacionados (Sant Llorenc del Munt, Eoceno, cuenca de antepaís surpirenaica)
López Blanco, M.; Piña, J.; Marzo, M. (Sociedad Geológica de España, 1994)High-resolution mapping and correlation of the syntectonic Sant Lloreng del Munt alluvial fan and fandelta deposits show that proximal alluvial fan sequences, d efined on the basis of sediment supply changes linked to ... -
Drenaje fluvial y topografía ligados a extensión: NÈ dé Iberia
Vergés i Masip, Jaume; Lewis, C.; Marzo, M. (Sociedad Geológica de España, 1996)Integrated analysis of fluvial drainage pattern, digital topography and regional tectonics allows to determine the lateral extent of high topography linked to the extensional system of faults that parallels the coastline ... -
Estratigrafía del llerdiense en la región de Tremp (cuenca de Graus-Tremp, NE de España)
Barberà, X.; Marzo, M.; Reguant, Salvador; Serra Kiel, Josep; Samsó, Josep Maria; Tosquella Angrill, Josep(Sociedad Geológica de España, 1996)
A new stratigraphic subdivision of the Herdian stratotype in the Tremp basin is proposed. The Figols Croup has been defined as a new unit which comprises a succession of shallow marine sediments about 750 m thick. This ... -
Hallazgo de Parotosuchus sp. (Amphibia, Temnospondyli) en las facies Buntsandstein del Pia de la Calma (Cordilleras Costeras Catalanas): resultados preliminares
Gaete, R.; Galobart, A.; Palomar, J.; Marzo, M. (Sociedad Geológica de España, 1994)The tetrapod fauna of La Mora site (Montseny massif) is located in the Buntsandstein facies at the lower part of the « Areniscas y lutitas del Figaró» unit. This fauna is found within a sandy, fluvial channel-fill and is ... -
Organización secuencial del sector occidental del abanico costero de Sant Llorenç del Munt (Eoceno, cuenca de antepaís surpirenaica)
López Blanco, M.; Marzo, M. (Sociedad Geológica de España, 1993)The study of the relationships among facies belts in the Eocene Sant Llorenç d el Munt fan-delta complex allow sus to differentia te three orders of transgressive-regressive cyclicity . The basic building blocks are the ... -
Precisiones estratigráficas sobre el límite inferior de la Formación Artés (Paleógeno, cuenca del Ebro)
López Blanco, M.; Piña, J.; Marzo, M. (Sociedad Geológica de España, 1994)According to its original definition, the Artes Formation is formed by the ensemble of continental, red mudstones and sandstones interbedded with conglomerates resting on top of the marine deposits of the Bartonian to ... -
Sedimentación lacustre y ciclicidad: las sucesiones fluvio-lacustres del Oligoceno superior del sector SE de la cuenca del Ebro
Barberà, X.; Cabrera, L.; Marzo, M.; Ripepe, M. (Sociedad Geológica de España, 1996)A cyclostratigraphic study of Late Oligocene fluvio-lacustrine and lacustrine sequences was carried out in the Ebro basin. Fourier spectral analysis was used to analyze four stratigraphic and sedimentological parameters ... -
Sedimentologia del sector occidental del abanico costerò de Sant Llorenf del Munt (Eoceno, cuenca de antepais surpirenaica)
López Blanco, M.; Marzo, M. (Sociedad Geológica de España, 1993)The Bartonian-Priabonian Sant Lloreng del Munt fan-delta complex is located at the SE margin of the South-Pyrenean foreland basin. During the deposition of this complex the basin margin was controlled by a series of sinistral ...