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Autor Liesa, Carlos L. |
Documentos disponibles escritos por este autor (4)
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texto impreso
Evidences of tectonic subsidence during the deposition of the marine Villarroya de los Pinares Formation (Aptian, Urgonian Facies) is found in the marginal Las Parras sub-basin (Maestrazgo Basin, Teruel). This tectonic activity is identified by [...]texto impreso
Rodríguez-López, Juan Pedro ; Liesa, Carlos L. ; Pardo, Gonzalo ; Meléndez Hevia, Nieves ; Soria, Ana R. ; Skilling, Ian | Elsevier | 2016-06-15The late Jurassic–early Cretaceous is commonly considered the only cold climatic interval in Earth history without any direct evidence of polar ice. A newly discovered dropstone-bearing interval from the subtropical Iberian Basin (western Tethys[...]texto impreso
A coastal siliciclastic unit was deposited during the Aptian at the base ofVillarroya de los Pinares Formation in Las Parras sub-basin. It can be subdivided in four coarsening-upwards coastal sequences. We focus in the third sequence (S3), which[...]texto impreso
Soria, Ana Rosa ; Liesa, Carlos L. ; Meléndez Hevia, Alfonso ; Meléndez Hevia, Nieves | Sociedad Geológica de España. | 2001The sedimentary record o f El Castellar Fm. in the Calve subbasin has been divided into two stages according to the presence of a mudstone and gypsum interval. This interval represents a paleogeographic and structural significative change. The g[...]