Stick-slip vs. stable sliding fault behaviour: A case-study using a multidisciplinary approach in the volcanic region of Mt. Etna (Italy)

Author:

Azzaro R.ORCID,Bonforte A.,D'Amico S.,Guglielmino F.,Scarfì L.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference79 articles.

1. Earthquake source scaling relationships from −1 to 5 ML using seismograms recorded at 2.5-km depth;Abercrombie;J. Geophys. Res.,1995

2. Seismological features of the Pernicana-Provenzana fault system (Mt. Etna, Italy) and implications for the dynamics of northeastern flank of the volcano;Alparone;J. Volc. Geotherm. Res.,2013

3. Buried active faults in the Zafferana Etnea territory (south-eastern flank of Mt. Etna): geometry and kinematics by earthquake relocation and focal mechanisms;Alparone;Ann. Geophys.,2013

4. Instrumental seismic catalogue of Mt Etna earthquakes (Sicily, Italy): ten years (2000−2010) of instrumental recordings;Alparone;Ann. Geophys.,2015

5. From geodetic imaging of seismic and aseismic fault slip to dynamic modeling of the seismic cycle;Avouac;Annu. Rev. Earth Planet. Sci.,2015

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