Australia's Moho: A test of the usefulness of gravity modelling for the determination of Moho depth
In general, seismic methods provide a reliable way to image the crust–mantle interface,
which is marked by a rapid increase in seismic velocity (the Moho). However, the coverage …
which is marked by a rapid increase in seismic velocity (the Moho). However, the coverage …
What drives A lpine T ethys opening? Clues from the review of geological data and model predictions
Permo‐Triassic remnants (300–220 Ma) of high‐temperature metamorphism associated
with large gabbro bodies occur in the Alps and indicate a high thermal regime compatible …
with large gabbro bodies occur in the Alps and indicate a high thermal regime compatible …
Integration of natural data within a numerical model of ablative subduction: a possible interpretation for the Alpine dynamics of the Austroalpine crust
A numerical modelling approach is used to validate the physical and geological reliability of
the ablative subduction mechanism during Alpine convergence in order to interpret the …
the ablative subduction mechanism during Alpine convergence in order to interpret the …
How lithospheric subduction changes along the Calabrian Arc in southern Italy: geophysical evidences
G Neri, AM Marotta, B Orecchio, D Presti… - International Journal of …, 2012 - Springer
Recent tomographic investigations performed down to~ 300 km depth in the Calabrian Arc
region gave insight in favor of the hypothesis that the Ionian subducting slab is continuous in …
region gave insight in favor of the hypothesis that the Ionian subducting slab is continuous in …
[HTML][HTML] From rifting to oceanization in the Gulf of Aden: Insights from 2D numerical models
We investigate the evolution of the Gulf of Aden from rift initiation to the development of
active oceanic spreading center by means of 2D thermo-mechanical numerical models, in …
active oceanic spreading center by means of 2D thermo-mechanical numerical models, in …
Formation and evolution of a subduction-related mélange: The example of the Rocca Canavese Thrust Sheets (Western Alps)
Abstract In the Sesia-Lanzo Zone, Western Alps, the Rocca Canavese Thrust Sheets (RCT)
subunit is characterized by a mixture of mantle-and crust-derived lithologies, such as …
subunit is characterized by a mixture of mantle-and crust-derived lithologies, such as …
Permian‐Triassic high thermal regime in the Alps: Result of late Variscan collapse or continental rifting? Validation by numerical modeling
The Permian‐Triassic igneous activity, associated with regional scale deformation
developed under high‐temperature/low‐pressure (HT‐LP) metamorphic conditions and …
developed under high‐temperature/low‐pressure (HT‐LP) metamorphic conditions and …
Metamorphic facies and deformation fabrics diagnostic of subduction: Insights from 2D numerical models
We developed a 2D numerical model that simulates the evolution of a subduction in order to
analyze which different metamorphic facies and deformation fabrics can be recorded within …
analyze which different metamorphic facies and deformation fabrics can be recorded within …
Gravity modelling of the Tyrrhenian-Calabrian-Ionian subduction system
This study provides a lithospheric-scale model along the Ionian Subduction zone in
Southern Italy, contributing to the seismotectonic investigation of a region which is affected …
Southern Italy, contributing to the seismotectonic investigation of a region which is affected …
[HTML][HTML] How many subductions in the Variscan orogeny? Insights from numerical models
We developed a 2D numerical model to simulate the evolution of two superposed ocean-
continent-ocean subduction cycles with opposite vergence, both followed by continental …
continent-ocean subduction cycles with opposite vergence, both followed by continental …