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  4. Present-day geodynamics in the bend of the western and central Alps as constrained by earthquake analysis
 
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Present-day geodynamics in the bend of the western and central Alps as constrained by earthquake analysis

Auteur(s)
Delacou, Bastien
Burkhard, Martin 
Centre d'hydrogéologie et de géothermie 
Champagnac, Jean-Daniel
Sue, Christian
Date de parution
2004
In
Geophysical Journal International, 2004/158/753-774
Mots-clés
  • Active tectonics
  • buoyancy forces
  • earthquake focal mecanisms
  • orogen-perpendicular extension
  • stress inversion
  • western/central Alps
  • Active tectonics

  • buoyancy forces

  • earthquake focal meca...

  • orogen-perpendicular ...

  • stress inversion

  • western/central Alps

Résumé
The contrasted tectonics of the western/central Alps is examined using a synthesis of 389 reliable focal mechanisms. The present-day strain regime is mapped and interpolated for the entire Alpine belt based on a newly developed method of regionalization. The most striking feature is a continuous area of extension which closely follows the large-scale topographic crest line of the Alpine arc. Thrusting is observed locally, limited to areas near the border of the Alpine chain. A majority of earthquakes within the Alps and its forelands are in strike-slip mode. Stress inversion methods have been applied to homogenous subsets of focal plane mechanisms in order to map regional variations in stress orientation. The stress state is confirmed to be orogen-perpendicular both for δ3 in the inner extensional zones and δ1 in the outer transcurrent/transpressional zones. Extensional areas are well correlated with the part of the belt which presents the thickest crust, as shown by the comparison with the Bouguer anomaly and the average topography of the belt. In the northwestern Swiss Alps, extension is also correlated with currently uplifting zones. These observations and our strain/stress analyses support a geodynamic model for the western Alps in which the current activity is mostly a result of gravitational 'body' forces. Earthquakes do not provide any direct evidence for ongoing convergence in the Alpine system, but a relationship with ongoing activity of complex block rotations of the Apulian microplate cannot be ruled out.
Identifiants
https://libra.unine.ch/handle/123456789/19174
_
10.1111/j.1365-246X.2004.02320.x
Type de publication
journal article
Dossier(s) à télécharger
 main article: 2_Delacou_Bastien_-_Present-day_geodynamics_in_the_bend_20050921120527-LO.pdf (5.56 MB)
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