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Structural evolution of the La Trocha fault zone: Oblique collision and strike-slip basins in the Cuban Orogen
ArticleAbstract: [1] The La Trocha fault zone acted as a major left-lateral transfer zone and is bounded by the La TrPalabras claves:Autores:Cruz-Orosa I., Ramos E., Rivero L., Sàbat F., Yaniel Misael Vázquez-TasetFuentes:scopusTectono-sedimentary evolution of transverse extensional faults in a foreland basin: Response to changes in tectonic plate processes
ArticleAbstract: Late Paleocene to Middle Eocene strata in the easternmost part of the Southern Pyrenees, up to 4 kmPalabras claves:evaporites, foreland basins, Iberia, Pyrenees, Sardinia, transverse faultsAutores:Casas A., Cox N., Emilio Carrillo, Guinea A., Rivero L., Yaniel Misael Vázquez-TasetFuentes:scopus