A Pedrera, J García-Senz, EL Pueyo, B López-Mir… - Earth-Science …, 2023 - Elsevier
The kinematic evolution of the Pyrenees was largely controlled by structural and thermal heterogeneities inherited from a precursor rift system, resulting in complex along-strike …
Assessing the size of a former ocean of which only remnants are found in mountain belts is challenging but crucial to understanding subduction and exhumation processes. Here we …
It is unanimously acknowledged that the Corsica‐Sardinia microplate rotated counterclockwise (CCW) by 40–50° between 21 and 15 Ma, synchronous with Liguro …
The nature and origin of the J‐magnetic anomaly along the Iberia–Newfoundland margins are controversial and its validity for plate kinematic reconstructions questioned. At present, it …
N Barnett‐Moore, DR Müller, S Williams, J Skogseid… - Basin …, 2018 - earthdoc.org
The stretched continental margins of the North Atlantic region record a plate kinematic history dominated by major episodes of extension since the Late Palaeozoic. Accounting for …
N Barnett‐Moore, M Hosseinpour, S Maus - Tectonics, 2016 - Wiley Online Library
Currently, there are several published end‐member plate models that describe the evolution of Iberia during the Mesozoic. We review key geological and geophysical data sets …
In this work we provide a reappraisal of the mid-Cretaceous extensional basins located to the east of the Pyrenean mountain ranges, from the easternmost portion of Iberia to the …
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 …
A global view of the Mesozoic-Cenozoic geodynamic evolution of the Iberian microplate is necessary to determine the role of inherited Variscan structures in the configuration of the …