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 …

The Society makes every effort to ensure that the scientific and production quality of its
books matches that of its journals. Since 1997, all book proposals have been refereed by …

Cretaceous rocks crop out extensively in the three main Alpine orogenic belts of Spain: the
Betic Cordillera, the Pyrenees and the Iberian Ranges. These rocks, deformed during …

The Concud fault is a 13.5 km long, NW–SE striking normal fault at the eastern Iberian
Chain. Its recent (Late Pleistocene) slip history is characterized from mapping and trench …

The present-day topography of the Iberian peninsula can be considered as the result of the
Mesozoic–Cenozoic tectonic evolution of the Iberian plate (including rifting and basin …

The stress evolution of the central-eastern Iberian Chain during the Tertiary compression
has been a matter of discussion during the last decades. In particular, there is not a …

Three regional joint sets striking N–S, E–W and WNW–ESE affect the Tertiary rocks of the
central Ebro basin. From analysis of their chronological relationships and spatial distribution …

Samples of non-striated fracture surfaces within clastic materials of Late Pliocene–
Pleistocene age from the Teruel grabens (eastern Spain) have been analysed using a stress …

Abstract The Teruel Basin is a NNE-SSW trending intracontinental extensional basin located
in central-eastern Iberia. It is asymmetrically bounded to the east by a major fault zone, but …

Abstract The NNW-SSE trending Teruel Basin rift is the largest Late Miocene-Quaternary
extensional intracontinental structure located within the central-eastern Iberian Chain …