Kinematics and geodynamics of crustal-block structures separated by compliant zones with viscoelastic rheology play an important role in defining the conditions for many deformation events such as ordinary seismic ruptures, silent and slow earthquakes and aseismic fault creep phenomena. New seismological data from the Latium-Abruzzi carbonatic platform of central Italy fit a block-tectonic modelling previously proposed for this area on the basis of structural and paleomagnetic evidences.

Bella, F., Caputo, M., DELLA MONICA, G., Lisi, A., Plastino, W., Scandone, R., et al. (1998). Crustal blocks and seismicity in the Central Apennines of Italy. IL NUOVO CIMENTO DELLA SOCIETÀ ITALIANA DI FISICA. C, GEOPHYSICS AND SPACE PHYSICS, 21(6), 597-607.

Crustal blocks and seismicity in the Central Apennines of Italy

PLASTINO, Wolfango;
1998-01-01

Abstract

Kinematics and geodynamics of crustal-block structures separated by compliant zones with viscoelastic rheology play an important role in defining the conditions for many deformation events such as ordinary seismic ruptures, silent and slow earthquakes and aseismic fault creep phenomena. New seismological data from the Latium-Abruzzi carbonatic platform of central Italy fit a block-tectonic modelling previously proposed for this area on the basis of structural and paleomagnetic evidences.
1998
Bella, F., Caputo, M., DELLA MONICA, G., Lisi, A., Plastino, W., Scandone, R., et al. (1998). Crustal blocks and seismicity in the Central Apennines of Italy. IL NUOVO CIMENTO DELLA SOCIETÀ ITALIANA DI FISICA. C, GEOPHYSICS AND SPACE PHYSICS, 21(6), 597-607.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11590/121268
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