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The Damage Assessment for Rapid Response (DARR) Method and its Application to Different Ground‐Motion Levels and Building Types
Estimating Cross‐Coupling in Site Response by Seismic Noise Interferometry: An Example from an Alpine Valley (Northeastern Italy)
On the Limitations of Spectral Source Parameter Estimation for Minor and Microearthquakes
Erratum to Near‐Real‐Time Damage Estimation for Buildings Based on Strong‐Motion Recordings: An Application to Target Areas in Northeastern Italy
Introduction to the Special Section on Advances in Site Response Estimation
Near‐Real‐Time Damage Estimation for Buildings Based on Strong‐Motion Recordings: An Application to Target Areas in Northeastern Italy
Site Amplification at Permanent Stations in Northeastern Italy
The 9 October 1963 Vajont Catastrophe from the Point of View of the WWSSN‐LP Recordings of the TRI‐117 Station, Trieste, Italy
The Antarctic Seismographic Argentinean Italian Network (ASAIN): Recording Earthquakes in the Scotia Sea Region
The OGS–Northeastern Italy Seismic and Deformation Network: Current Status and Outlook
Rapid Damage Scenario Assessment for Earthquake Emergency Management
Could a Decentralized Onsite Earthquake Early Warning System Help in Mitigating Seismic Risk in Northeastern Italy? The Case of the 1976 M s 6.5 Friuli Earthquake
Seasonality in Site Response: An Example from Two Historical Earthquakes in Kazakhstan
Volcanic activities triggered or inhibited by resonance of volcanic edifices to large earthquakes
Bayesian Estimation of Macroseismic Intensity from Post-Earthquake Rapid Damage Mapping
κ 0 : Origin and Usability
Performance of the GFZ Decentralized On‐Site Earthquake Early Warning Software (GFZ‐Sentry): Application to K‐NET and KiK‐Net Recordings, Japan
Abstract The knowledge of the largest expected earthquake magnitude in a region is one of the key issues in probabilistic seismic hazard calculations and the estimation of worst-case scenarios. Earthquake catalogues are the most informative source of information for the inference of earthquake magnitudes. We analysed the earthquake catalogue for Central Asia with respect to the largest expected magnitudes m T in a pre-defined time horizon T f using a recently developed statistical methodology, extended by the explicit probabilistic consideration of magnitude errors. For this aim, we assumed broad error distributions for historical events, whereas the magnitudes of recently recorded instrumental earthquakes had smaller errors. The results indicate high probabilities for the occurrence of large events (M≥8), even in short time intervals of a few decades. The expected magnitudes relative to the assumed maximum possible magnitude are generally higher for intermediate-depth earthquakes (51–300 km) than for shallow events (0–50 km). For long future time horizons, for example, a few hundred years, earthquakes with M≥8.5 have to be taken into account, although, apart from the 1889 Chilik earthquake, it is probable that no such event occurred during the observation period of the catalogue.