“The characterization of seismogenic sources and the process of determining the seismic coupling require knowledge of the seismogenic lithosphere’s thickness, which is bounded by upper and lower seismogenic depth. This study, based on two updated earthquake catalogues for the transition zone between the Alps, Dinarides and Pannonian Basin, explores the variability of seismogenic depth and seismic coupling to be included in the new Slovenian seismic hazard model.”
Zupančič et al, 2024, Natural Hazards and Earth System Sciences
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