Magma chambers and localization of deformation during thrusting. (Articolo in rivista)

Type
Label
  • Magma chambers and localization of deformation during thrusting. (Articolo in rivista) (literal)
Anno
  • 2010-01-01T00:00:00+01:00 (literal)
Alternative label
  • Montanari D.; Corti G.; Simakin A. (2010)
    Magma chambers and localization of deformation during thrusting.
    in TERRA nova (Print)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Montanari D.; Corti G.; Simakin A. (literal)
Pagina inizio
  • 390 (literal)
Pagina fine
  • 395 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 22 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#note
  • In: Terra Nova, vol. 22 (5) pp. 390 - 395. Blackwell, 2010. (literal)
Note
  • ISI Web of Science (WOS) (literal)
Titolo
  • Magma chambers and localization of deformation during thrusting. (literal)
Abstract
  • We present the results of coupled analogue and numerical models that provide new insights into the relationships between volcanoes and thrusts. The effects of both upper-crustal magma chambers and the load of volcanoes on the geometry of thrust systems were investigated. Analogue modelling points to a strong influence exerted by a magma chamber on thrust geometry, which, as suggested by the numerical models used to rationalize these results, is related to the stress redistribution around the weak heterogeneity. The low-viscosity body below a volcanic edifice localizes compressional deformation and causes a curvature of the thrusts towards the magma chamber, opposite to the direction of tectonic transport. In these conditions, the volcanic load has a negligible effect on the structural geometry. These results are in contrast with those of previous studies, where intrusions or the load of major volcanoes generated a curvature of the thrusts away from volcanic edifices in the direction of tectonic transport. (literal)
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