La evolución temporal de los minerales de 1a arcilla en el Pérmico superior y Triásico de Cuenca y Teruel (Cordillera Ibérica SE).

1. Alonso Azcárate, Jacinto
2. Arche Miralles, Alfredo
3. Fernández Barrenechea, José María
4. López Gómez, José
5. Luque, F. J.
6. Rodas González, Magdalena

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lock_openArias Montano externo

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Otras publicaciones en: Geogaceta

Resumen

Clay mineralogy of the continetal and shallow marine sediments of Permian and Triassic age of the SE Iberian Ranges is a neglected subject. The present study shows the temporal variations of clay mineral assemblages and point out to two main primary controls: nature of the source area and sedimentary environments. Later diagenetic processes have not altered substantially the original mineralogy

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