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- W2077567522 abstract "espanolLa Cordillera Iberica es una cadena intraplaca originada por la compresion alpina durante el Paleogeno- Mioceno inferior. El relieve construido inicialmente por la orogenia se conserva en su mitad noroccidental en forma de macizos elevados asociados a grandes pliegues y cabalgamientos (Cameros, Moncayo, Sierra de Albarracin), si bien las estructuras compresivas fueron casi arrasadas en muchas areas por extensas superficies de aplanamiento neogenas. En el sector centro-oriental el relieve fue modificado por la tectonica extensional del Mioceno superior-Cuaternario, formandose las depresiones de Teruel, Jiloca, Sarrion y Maestrat. El papel relativo de esta etapa tectonica y de la compresion anterior en el levantamiento de los macizos que separan dichas depresiones (Gudar, Javalambre) es aun una cuestion controvertida. El ‘esculpido’ final de los relieves tectonicos se debe a la incision de la red fluvial durante el Plioceno-Cuaternario, con el consiguiente desarrollo de modelados estructurales en los sustratos de Fuertes contrastes litologicos. EnglishThe intraplate Iberian Chain was originated by alpine, Palaeogene to Early Miocene compression. The relief initially built by the orogeny still remains in the north-western half of the chain in the form of high massifs associated to large folds and thrusts (Cameros, Moncayo, Sierra de Albarracin), although the compressive structures were almost completely levelled by vast Neogene erosion surfaces in large areas. In the central-eastern sector the relief was modified by extensional tectonics during late Miocene to Quaternary times, giving rise to the Teruel, Jiloca, Sarrion and Maestrat depressions. The relative role of this tectonic process and the previous compressive one in building the massifs which separate those depressions (Gudar, Javalambre) is still a controversial issue. The final modelling of tectonic relief is due to river incision during Pliocene and Quaternary times, with subsequent development of structural modelling on geologic substrata with strong lithologic contrasts." @default.
- W2077567522 created "2016-06-24" @default.
- W2077567522 creator A5011561803 @default.
- W2077567522 date "2007-01-01" @default.
- W2077567522 modified "2023-09-26" @default.
- W2077567522 title "La construcción y el modelado dels relieve en la Cordillera Ibérica" @default.
- W2077567522 hasPublicationYear "2007" @default.
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