[HTML][HTML] Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic
The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
Crustal structure and evolution of the Pyrenean-Cantabrian belt: A review and new interpretations from recent concepts and data
This paper provides a synthesis of current data and interpretations on the crustal structure of
the Pyrenean-Cantabrian orogenic belt, and presents new tectonic models for …
the Pyrenean-Cantabrian orogenic belt, and presents new tectonic models for …
[HTML][HTML] Kinematics and extent of the Piemont–Liguria Basin–implications for subduction processes in the Alps
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 …
challenging but crucial to understanding subduction and exhumation processes. Here we …
Kinematic evolution of the southern North Atlantic: Implications for the formation of hyperextended rift systems
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 …
propagation of deformation in hyperextended rift systems using plate kinematic modeling …
Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary
P Angrand, F Mouthereau - BSGF-Earth Sciences …, 2021 - pubs.geoscienceworld.org
Abstract The West European collisional Alpine belts are the result of the inversion, initiated
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
[HTML][HTML] A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
The western European kinematic evolution results from the opening of the western
Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological …
Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological …
A new southern North Atlantic isochron map: Insights into the drift of the Iberian plate since the Late Cretaceous
This paper presents a new southern North Atlantic plate model from Late Cretaceous to
present, with the aim of constraining the kinematics of the Iberian plate during the last 83.5 …
present, with the aim of constraining the kinematics of the Iberian plate during the last 83.5 …
The Mesozoic Iberia-Eurasia diffuse plate boundary: A wide domain of distributed transtensional deformation progressively focusing along the North Pyrenean Zone
Plate kinematic reconstructions available for the Late Jurassic-Early Cretaceous eastward
drift and counterclockwise rotation of the Iberian plate imply a major left-lateral motion of …
drift and counterclockwise rotation of the Iberian plate imply a major left-lateral motion of …
Alpine orogeny: Deformation and structure in the northern Iberian margin (Pyrenees sl)
JA Muñoz - The Geology of Iberia: A Geodynamic Approach …, 2019 - Springer
Abstract The Pyrenean Orogenic system formed by the contractional deformation of the
North Iberian margin from late Santonian to Middle Miocene times as a result of the collision …
North Iberian margin from late Santonian to Middle Miocene times as a result of the collision …
Continental break-up of the South China Sea stalled by far-field compression
The outcome of decades of two-dimensional modelling of lithosphere deformation under
extension is that mechanical coupling between the continental crust and the underlying …
extension is that mechanical coupling between the continental crust and the underlying …