Articles | Volume 52
https://doi.org/10.5194/adgeo-52-145-2021
https://doi.org/10.5194/adgeo-52-145-2021
19 Mar 2021
 | 19 Mar 2021

Topography and structural heterogeneities in surface ground deformation: a simulation test for Somma-Vesuvius volcano

Umberto Tammaro, Umberto Riccardi, Vittorio Romano, Michele Meo, and Paolo Capuano

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Cited articles

Bianco, F., Castellano, M., Milano, G., Ventura, G., and Vilardo, G.: The Somma-Vesuvius stress field induced by regional tectonics: Evidences from seismological and mesostructural data, in: Special Issue Vesuvius, edited by: Spera, F. J., De Vivo, B., Ayuso, R. A., and Belkin, H. E., J. Volcanol. Geoth. Res., 82, 199–218, https://doi.org/10.1016/S0377-0273(97)00065-6, 1998. 
Bianco, F., Castellano, M., Milano, G., Vilardo, G., Ferrucci, F., and Gresta, S.: The seismic crises at Mt. Vesuvius during 1995 and 1996, Phys. Chem. Earth (A), 24, 977–983, 1999. 
Capuano, P., Gasparini, P., Virieux, J., Zollo, A., Casale, R., and Yeroyanni, M.: The Internal Structure of Mt. Vesuvius: A Seismic Tomography Investigation, Liguori Editore, Napoli, 595 pp., ISBN 88-207-3503-2, 2003. 
Capuano, P., Russo, G., and Scarpa, R.: P-wave velocity and density structure beneath Mt. Vesuvius: a magma body in the upper edifice?, Ann. Geophys.-Italy, 54, S0437–S0447, https://doi.org/10.4401/ag-6443, 2013. 
Chiodini, G., Marini, L., and Russo, M.: Geochemical evidences of high temperature hydrothermal brines at Vesuvio volcano (Italy), Geochim. Cosmochim. Ac., 65, 2129–2147, 2001. 
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We simulate the deformation of Somma-Vesuvius volcano due to some overpressure sources by means of a finite element 3D code. The goal of these simulations is to investigate the influence of topography and structural heterogeneity on ground deformation. The results suggest that they are key factors governing the ground deformation. Our study clearly demonstrate that a better knowledge of deformation patterns can significantly help in the design of an efficient geodetic network.
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