[HTML][HTML] EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region
IM Artemieva, H Thybo - Tectonophysics, 2013 - Elsevier
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 …
A review on the driving mechanism of the Tyrrhenian–Apennines system: Implications for the present seismotectonic setting in the Central-Northern Apennines
E Mantovani, D Babbucci, C Tamburelli, M Viti - Tectonophysics, 2009 - Elsevier
The formation of the Tyrrhenian–Apennines system has been characterized by a complex
distribution of major tectonic events, such as opening of basins, migration and distortion of …
distribution of major tectonic events, such as opening of basins, migration and distortion of …
The Moho depth map of the European Plate
M Grad, T Tiira… - Geophysical journal …, 2009 - academic.oup.com
Summary The European Plate has a 4.5 Gy long and complex tectonic history. This is
reflected in the present-day large-scale crustal structures. A new digital Moho depth map is …
reflected in the present-day large-scale crustal structures. A new digital Moho depth map is …
Contrasting styles of (U) HP rock exhumation along the Cenozoic Adria‐Europe plate boundary (Western Alps, Calabria, Corsica)
Since the first discovery of ultrahigh pressure (UHP) rocks 30 years ago in the Western Alps,
the mechanisms for exhumation of (U) HP terranes worldwide are still debated. In the …
the mechanisms for exhumation of (U) HP terranes worldwide are still debated. In the …
Subduction, convergence and the mode of backarc extension in the Mediterranean region
35 Ma ago a major change occurred in the Mediterranean region, from a regionally
compressional subduction coeval with the formation of Alpine mountain belts, to extensional …
compressional subduction coeval with the formation of Alpine mountain belts, to extensional …
Timing, thrusting mode, and negative inversion along the Circeo thrust, Apennines, Italy: How the accretion‐to‐extension transition operated during slab rollback
The evolution of the Apennine wedge has seen the time‐space migration of the forebulge,
foredeep, thrust wedge, and back‐arc extension phases in the wake of the Eastward …
foredeep, thrust wedge, and back‐arc extension phases in the wake of the Eastward …
Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-field versus far-field interactions
The present-day tectonic setting of the Western Mediterranean region, from the Pyrénées to
the Betics and from the Alps to the Atlas, results from a complex 3-D geodynamic evolution …
the Betics and from the Alps to the Atlas, results from a complex 3-D geodynamic evolution …
Beginning of the Apennine subduction system in central western Mediterranean: Constraints from Cenozoic “orogenic” magmatic activity of Sardinia, Italy
Major and trace element analyses plus six new 40Ar/39Ar data obtained on feldspar
separates for selected igneous rocks belonging to the Oligo‐Miocene igneous activity of …
separates for selected igneous rocks belonging to the Oligo‐Miocene igneous activity of …
[HTML][HTML] Transfer zones in Mediterranean back-arc regions and tear faults
Slab tearing induces localized deformations in the overriding plates of subduction zones
and transfer zones accommodating differential retreat in back-arc regions. Because the …
and transfer zones accommodating differential retreat in back-arc regions. Because the …
Continental breakup and the dynamics of rifting in back‐arc basins: The Gulf of Lion margin
Deep seismic profiles and subsidence history of the Gulf of Lion margin reveal an intense
stretching of the distal margin and strong postrift subsidence, despite weak extension of the …
stretching of the distal margin and strong postrift subsidence, despite weak extension of the …