Slow rupture of an aseismic fault in a seismogenic region of Central Italy
Slow earthquakes and afterslips prove that the Earth does not have just two response time scales, i.e. that of tectonic loading and that of regular earthquakes. A swarm of slow earthquakes, with time constants of the order of hundreds of seconds, has been detected by a laser interferometer below the Gran Sasso massif (Italy). We analyse and model
Amoruso, Antonella et al.
Fecha de publicación:
12
2002