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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Zambia
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Asia
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Primary terms
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Africa
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Italy
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intermediate-focus earthquakes
Potential link between antigorite dehydration and shallow intermediate-depth earthquakes in hot subduction zones
Double Seismic Zones along the Eastern Aleutian‐Alaska Subduction Zone Revealed by a High‐Precision Earthquake Relocation Catalog
Ground-motion models for Vrancea intermediate-depth earthquakes
Geotechnical lessons from the M w 7.1 2018 Anchorage Alaska earthquake
Ground-motion model for subduction earthquakes in northern South America
Loreto Intermediate Depth Earthquake of 26 May 2019 (Northeast Peru): Source Parameters by Inversion of Local to Regional Waveforms and Strong‐Motion Observations
Ground‐Motion Duration Prediction Model from Recorded Mexican Interplate and Intermediate‐Depth Intraslab Earthquakes
Updated ground motion prediction model for Mexican intermediate-depth intraslab earthquakes including V / H ratios
Advances in the thermal and petrologic modeling of subduction zones
Stochastic Strong Ground Motion Simulation of the Southern Aegean Sea Benioff Zone Intermediate‐Depth Earthquakes
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.