Rifted margin architecture and crustal rheology: reviewing Iberia-Newfoundland, central South Atlantic, and South China Sea
Crustal rheology controls the style of rifting and ultimately the architecture of rifted margins.
Here we review the formation of three magma-poor margin pairs, Iberia-Newfoundland, the …
Here we review the formation of three magma-poor margin pairs, Iberia-Newfoundland, the …
[HTML][HTML] EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region
We present a new digital crustal model for Moho depth and crustal structure in Europe,
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …
Rift migration explains continental margin asymmetry and crustal hyper-extension
When continents break apart, continental crust and lithosphere are thinned until break-up is
achieved and an oceanic basin is formed. The most remarkable and least understood …
achieved and an oceanic basin is formed. The most remarkable and least understood …
EPcrust: a reference crustal model for the European Plate
We present a new crustal model for the European Plate, derived from collection and critical
integration of information selected from the literature. The model covers the whole European …
integration of information selected from the literature. The model covers the whole European …
How does the continental crust thin in a hyperextended rifted margin? Insights from the Iberia margin
E Sutra, G Manatschal - Geology, 2012 - pubs.geoscienceworld.org
The discovery of hyperthinned continental crust and exhumed mantle on present-day deep-
water rifted margins leads to two fundamental questions:(1) in detail, how does the crust thin …
water rifted margins leads to two fundamental questions:(1) in detail, how does the crust thin …
Slab rupture and delamination under the Betics and Rif constrained from receiver functions
We map the lithospheric structure under the westernmost Mediterranean convergent setting
interpreting P-receiver functions obtained from a dense seismic network. No orogenic root …
interpreting P-receiver functions obtained from a dense seismic network. No orogenic root …
The structure and evolution of the lithosphere–asthenosphere boundary beneath the Atlantic–Mediterranean Transition Region
The present-day thermal and compositional 3D structure of the lithosphere beneath the
Atlantic–Mediterranean Transition Region and the lithosphere–asthenosphere interaction …
Atlantic–Mediterranean Transition Region and the lithosphere–asthenosphere interaction …
Finite‐frequency Rayleigh wave tomography of the western Mediterranean: Map** its lithospheric structure
We present a 3‐D shear wave velocity model for the crust and upper mantle of the western
Mediterranean from Rayleigh wave tomography. We analyzed the fundamental mode in the …
Mediterranean from Rayleigh wave tomography. We analyzed the fundamental mode in the …
Seismic velocity model of the crust and upper mantle along profile PANCAKE across the Carpathians between the Pannonian Basin and the East European Craton
V Starostenko, T Janik, K Kolomiyets, W Czuba… - Tectonophysics, 2013 - Elsevier
Results are presented of a seismic wide-angle reflection/refraction survey along a profile
between the Pannonian Basin (PB) and the East European Craton (EEC) called PANCAKE …
between the Pannonian Basin (PB) and the East European Craton (EEC) called PANCAKE …
Insights into the crustal‐scale dynamics of a doubly vergent orogen from a quantitative analysis of its forelands: A case study of the Eastern Pyrenees
In natural doubly vergent orogens, the relationship between the pro‐and retro‐wedges is, as
yet, poorly constrained. We present a detailed tectonostratigraphic study of the retro‐wedge …
yet, poorly constrained. We present a detailed tectonostratigraphic study of the retro‐wedge …