Relocation of earthquakes in the southern and eastern Alps (Austria, Italy) recorded by the dense, temporary SWATH-D network using a Markov chain Monte Carlo inversion
Azam Jozi Najafabadi et al.
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Total article views: 1,968 (including HTML, PDF, and XML)
Thereof 1,869 with geography defined
and 99 with unknown origin.
Total article views: 1,332 (including HTML, PDF, and XML)
Thereof 1,262 with geography defined
and 70 with unknown origin.
Total article views: 636 (including HTML, PDF, and XML)
Thereof 607 with geography defined
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This study achieved high-precision hypocenters of 335 earthquakes (1–4.2 ML) and 1D velocity models of the Southern and Eastern Alps. The general pattern of seismicity reflects head-on convergence of the Adriatic Indenter with the Alpine orogenic crust. The relatively deeper seismicity in the eastern Southern Alps and Giudicarie Belt indicates southward propagation of the Southern Alpine deformation front. The derived hypocenters form excellent data for further seismological studies, e.g., LET.
This study achieved high-precision hypocenters of 335 earthquakes (1–4.2 ML) and 1D velocity...