A naturally constrained stress profile through the middle crust in an extensional terrane
We present a method in which paleopiezometry, Ti-in-quartz thermobarometry (TitaniQ), and
2-D thermal modeling are used to construct a naturally constrained stress profile through the …
2-D thermal modeling are used to construct a naturally constrained stress profile through the …
From Permo-Triassic lithospheric thinning to Jurassic rifting at the Adriatic margin: Petrological and geochronological record in Valtournenche (Western Italian Alps)
Slices of polycyclic metasediments (marbles and meta-cherts) are tectonically amalgamated
with the polydeformed basement of the Dent Blanche tectonic system along a major Alpine …
with the polydeformed basement of the Dent Blanche tectonic system along a major Alpine …
Continental interior and edge breakup at convergent margins induced by subduction direction reversal: A numerical modeling study applied to the South China Sea …
The dynamics of continental breakup at convergent margins has been described as the
results of backarc opening caused by slab rollback or drag force induced by subduction …
results of backarc opening caused by slab rollback or drag force induced by subduction …
[HTML][HTML] The role of structural inheritance in continental break-up and exhumation of Alpine Tethyan mantle (Canavese Zone, Western Alps)
Abstract The Canavese Zone (CZ) in the Western Alps represents the remnant of the distal
passive margin of the Adria microplate, which was stretched and thinned during the Jurassic …
passive margin of the Adria microplate, which was stretched and thinned during the Jurassic …
The transition from Variscan collision to continental break-up in the Alps: Insights from the comparison between natural data and numerical model predictions
Records of Variscan structural and metamorphic imprints in the Alps indicate that before
Pangaea fragmentation, the continental lithosphere was thermally and mechanically …
Pangaea fragmentation, the continental lithosphere was thermally and mechanically …
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 …
[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 …
Structural Architecture and Attenuation of the Ductile Lower Plate of the Ruby Mountain‐East Humboldt Range Metamorphic Core Complex, Northeast Nevada
Strongly deformed footwall rocks exposed in metamorphic core complexes (MCC) of the
North American Cordillera were exhumed via ductile attenuation, mylonitic shearing, and …
North American Cordillera were exhumed via ductile attenuation, mylonitic shearing, and …
Strain localization, granulite formation and geodynamic setting of 'hot orogens': a case study from the Eastern Ghats Province, India
S Gupta - Geological Journal, 2012 - Wiley Online Library
The Eastern Ghats Province underwent major orogenic events in the Neoproterozoic–
Cambrian period: 980–930, 900–650 and 550–500 Ma. At each time interval, deformation …
Cambrian period: 980–930, 900–650 and 550–500 Ma. At each time interval, deformation …