At plate boundaries, where deformation is localized along centimetre-to kilometre-scale shear zones, the influence of serpentinite on tectonic processes is linked to its unique …
F Sapin, JC Ringenbach, C Clerc - Scientific Reports, 2021 - nature.com
Rifted margins are the result of the successful process of thinning and breakup of the continental lithosphere leading to the formation of new oceanic lithosphere. Observations on …
Abstract The Bay of Biscay and the Pyrenees correspond to a Lower Cretaceous rift system including both oceanic and hyperextended rift domains. The transition from preserved …
Rifted margins are formed by persistent stretching of continental lithosphere until breakup is achieved. It is well known that strain-rate-dependent processes control rift evolution,, yet …
Estimating shortening in collision belts is critical to reconstruct past plate motions. Balanced cross‐section techniques are efficient in external domains but lack resolution in the …
We focus on the southern North Atlantic rifted margins to investigate the partitioning and propagation of deformation in hyperextended rift systems using plate kinematic modeling …
Abstract The South China Sea margins represent a critical natural laboratory to study the processes and parameters controlling the rift-to-drift transition. High quality seismic data …
G Manatschal, L Lavier, P Chenin - Gondwana Research, 2015 - Elsevier
A long-standing question in Earth Sciences is related to the importance of inheritance in controlling tectonic processes. In contrast to physical processes that are generally …