Finite element analysis of ground deformation due to dike intrusion with applications to Mt. Etna volcano
Item
Title (Dublin Core)
Finite element analysis of ground deformation due to dike intrusion with applications to Mt. Etna volcano
Description (Dublin Core)
A 2D finite elements study was carried out to analyse the effects caused by dike intrusion inside a heterogeneous medium and with a realistic topography of Mt. Etna volcano. Firstly, the method (dimension domain, elements type) was calibrated using plane strain models in elastic half-spaces; the results were compared with those obtained from analytical dislocation models. Then the effects caused both by the topographic variations and the presence of multi-layered medium on the surface, were studied. In particular, an application was then considered to Mt. Etna by taking into account the real topography and the stratification deduced from seismic tomography. In these conditions, the effects expected by the dike, employed to model the 2001 eruption under simple elastic half-space medium conditions, were computed, showing that topography is extremely important, at least in the near field.
Creator (Dublin Core)
G. La Rosa
A. Bonaccorso
M. Elia
A. Occhipinti Amato
Subject (Dublin Core)
FEM
ground deformation
dike intrusion
real medium
Meteorology. Climatology
QC851-999
Geophysics. Cosmic physics
QC801-809
Publisher (Dublin Core)
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
Date (Dublin Core)
2004-06-01T00:00:00Z
Type (Dublin Core)
article
Identifier (Dublin Core)
10.4401/ag-3357
1593-5213
2037-416X
https://doaj.org/article/c12d55996c204a31b27ad3bf2e10cd49
Source (Dublin Core)
Annals of Geophysics, Vol 47, Iss 5 (2004)
Language (Dublin Core)
EN
Relation (Dublin Core)
http://www.annalsofgeophysics.eu/index.php/annals/article/view/3357
https://doaj.org/toc/1593-5213
https://doaj.org/toc/2037-416X
Provenance (Dublin Core)
Journal Licence: CC BY