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The traditional view of the rheology of the continental lithosphere, sometimes known as the “jelly sandwich model”, consists of a strong upper crust, a weak lower crust, and a strong upper lithospheric mantle. Some authors argue, however, that t[...]texto impreso
Ruíz, A. M. ; Ferhat, G. ; Alfaro, Pedro ; Sanz De Galdeano-Equiza, Carlos ; Lacy de, María Clara ; Rodríguez Caderot, Gracia ; Gil, Antonio José | Elsevier Science B.V | 2003-04The Granada basin, located in the central sector of the Betic Cordillera, is one of the most seismically active zones of the Iberian Peninsula. For the first time, a geodetic network along the Padul fault and two levelling profiles (Genil and Vi[...]texto impreso
The Iberian Basin was an intracratonic rift basin in central-eastern Spain developed since Early Permian times. The basin boundary faults were normal, listric faults controlling an asymmetric extension propagating northeast with time. Hercynian [...]texto impreso
The Eslida Fm is an alluvial unit of the Buntsandstein Facies of the Iberian Ranges deposited in a half-graben basin over a period of 2–2.5 Ma during the lower Anisian (Middle Triassic). It can be subdivided into six cycles that can be correlate[...]texto impreso
Wees, Jan Dierik van ; Arche, Alfredo ; Beijdorff, C.G. ; López Gómez, José ; Cloetingh, Sierd A.P.L. | Elsevier Science B.V | 1998By subsidence analysis on eighteen surface sections and 6 wells, which cover large part of the Iberian Basin (E Spain) and which are marked by high-resolution stratigraphy of the Permian, Triassic, Jurassic and Cretaceous, we quantify the comple[...]texto impreso
Jiménez Díaz, Alberto ; Ruiz Pérez, Javier ; Villaseca González, Carlos ; Tejero López, Rosa ; Capote del Villar, Ramón | Elsevier Science B.V | 2012In this work we have modeled the thermal structure of the lithosphere of the Spanish Central System and the Tajo Basin, and their implications for lithospheric strength. For his, we have used refined heatproducing elements (HPE) values to obtai[...]
