Westward propagation of postorogenic rifting in the central sector of the Iberian Chain
generated the Teruel and Calatayud Mio-Pliocene grabens and the Jiloca, Daroca and …

In tectonically active areas, the landscape response to tectonic forcing is described and
possibly quantified by regional topographic and hydrographic features as well as by spatial …

Several grabens superimposed on the previous contractional structures have been
developed in the central sector of the Iberian &KDLQ GXULQJ WKH SRVW RURJHQLF …

The Jiloca depression, one of the largest morpho-structural units of the Iberian Range and
traditionally considered as a neotectonic graben, is interpreted as a karst polje developed …

Abstract The Iberian Chain (central–eastern Spain) is characterized by a dome-shaped
topography with poorly incised and relatively flat landscape in its interior at an elevation of …

The Jiloca basin is a large intramontane, NNW–SSE-trending topographical depression in
which the relative role of tectonic subsidence and erosional lowering is currently a matter of …

In the Central Iberian Chain (Spain), covering an area of some 7400 km2, up to seven
stepped erosion surfaces are determined from aerial photographs and field observations …

The seismogenic potential of active faults for seismic hazard analyses are typically
constrained using slip rates. These parameters, derived from numerically dated Quaternary …

The official seismic hazard models in Spain used in the seismic building codes do not
incorporate Quaternary faults, largely due to insufficient data for their proper …

Abstract Diagenesis of Miocene-Pliocene continental rocks in extensional Teruel Basin
related to deposition of a travertine at surface has been studied. Most of the diagenetic …