Abstract During the Late Jurassic and Early Cretaceous, Iberia experienced extensional and transtensional stresses leading to a complex rifting time interval. Africa–America–Europe …
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 …
Large‐scale faults in the continental crust are significant features that control the evolution of sedimentary basins and intraplate mountain chains. Deciphering their evolution is a …
In the Galve sub-basin, the sedimentary record of the Upper Hauterivian–Lower Barremian El Castellar Formation is divided into two stages by a marlstone interval with gypsum. Stage …
The Montsec unit is one of the most important detached South-verging nappes within the South Pyrenean Central Unit (SPCU, Southern Pyrenees). AN–S cross-section of its …
Many works in the last decades underline the role of evaporites, not just as a conditioning factor but as the engine for subsidence and eventually basin inversion. The western …
Abstract The late Jurassic–early Cretaceous is commonly considered the only cold climatic interval in Earth history without any direct evidence of polar ice. A newly discovered …
La Cordillera Ibérica es una cadena intraplaca formada durante el Paleógeno-Mioceno inferior a partir de la inversión de la Cuenca Ibérica extensional mesozoica a partir de …
A review of the onset of the synrift sedimentation and synsedimentary extensional tectonics of the Oliete sub-basin (northwestern Maestrazgo basin, East Spain) is presented here …