[HTML][HTML] Fluid evolution from extension to compression in the Pyrenean Fold Belt and Basque-Cantabrian Basin: A review
We propose a review to discuss the large number of studies dealing with the fluid history in
extensional and compressional sedimentary basins that evolved along the Iberian-Eurasian …
extensional and compressional sedimentary basins that evolved along the Iberian-Eurasian …
Tethys–Atlantic interaction along the Iberia–Africa plate boundary: The Betic–Rif orogenic system
J Vergés, M Fernàndez - Tectonophysics, 2012 - Elsevier
Initial SE-dipping slow subduction of the Ligurian–Tethys lithosphere beneath Africa from
Late Cretaceous to middle Oligocene twisting to a later faster E-dipping subduction of the …
Late Cretaceous to middle Oligocene twisting to a later faster E-dipping subduction of the …
Placing limits to shortening evolution in the Pyrenees: Role of margin architecture and implications for the Iberia/Europe convergence
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 …
cross‐section techniques are efficient in external domains but lack resolution in the …
[图书][B] Sediment routing systems: The fate of sediment from source to sink
PA Allen - 2017 - books.google.com
This cutting-edge summary combines ideas from several sub-disciplines including geology,
geomorphology, oceanography and geochemistry to provide an integrated view of Earth …
geomorphology, oceanography and geochemistry to provide an integrated view of Earth …
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 …
The Qs problem: Sediment volumetric balance of proximal foreland basin systems
Although the stratigraphy of sedimentary basins depends on the balance between the
magnitude and grain‐size characteristics of the sediment supply (Qs) and the spatial …
magnitude and grain‐size characteristics of the sediment supply (Qs) and the spatial …
[PDF][PDF] The structure of the South-Central-Pyrenean fold and thrust belt as constrained by subsurface data
Structural style of fold and thrust belts depends among many other factors on the mechanical
properties of the deformed sedimentary pile and the existence of weak horizons such as salt …
properties of the deformed sedimentary pile and the existence of weak horizons such as salt …
From salt‐bearing rifted margins to fold‐and‐thrust belts. Insights from analog modeling and Northern Calcareous Alps case study
P Santolaria, P Granado, EP Wilson, M de Matteis… - …, 2022 - Wiley Online Library
Analog modeling is used to study the role played by the inherited salt‐sediment architecture
of a salt‐bearing rifted margin, developed by minibasin downbuilding and margin‐scale …
of a salt‐bearing rifted margin, developed by minibasin downbuilding and margin‐scale …
Paleogeographic and sedimentary evolution of the South Pyrenean foreland basin
Abstract During the Paleogene and Neogene the NE Iberian plate underwent significant
paleogeographic changes driven by the Iberian and European plate collision and the …
paleogeographic changes driven by the Iberian and European plate collision and the …
Denudation history and palaeogeography of the Pyrenees and their peripheral basins: an 84-million-year geomorphological perspective
This review provides a synthesis of the evolution of the Pyrenees since~ 84 Ma and is
uniquely focused on analysing jointly and comparatively its peripheral pro-foreland, retro …
uniquely focused on analysing jointly and comparatively its peripheral pro-foreland, retro …