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Probabilistic Seismic Hazard Assessment of Armenia Using an Integrated Seismotectonic Framework
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Armenia is located within the central segment of the Arabia–Eurasia continental collision zone and is exposed to significant seismic hazard. This study presents an updated probabilistic seismic hazard assessment (PSHA) for Armenia based on an integrated seismotectonic framework incorporating active fault data, paleoseismological evidence, and historical and instrumental seismicity. A hybrid seismic source model was developed by combining fault-based characteristic earthquake sources with distributed background seismicity. Hazard calculations were performed using the OpenQuake engine within a logic-tree framework to account for epistemic uncertainties in earthquake occurrence and ground-motion prediction. Ground motion was estimated using a weighted set of ground motion prediction equations (GMPEs). Peak ground acceleration (PGA) hazard maps were computed for several return periods, with emphasis on the 475-year return period (10% probability of exceedance in 50 years). The results indicate PGA values across Armenia ranging from approximately 0.2 g to 0.5 g, with the highest hazard levels in northwestern Armenia along the Pambak–Sevan–Syunik Fault System. Hazard deaggregation shows that seismic hazard in major Armenian cities is primarily controlled by shallow earthquakes with magnitudes Mw 6.8–7.4 occurring within ~30 km of urban centers. The results provide a scientific basis for seismic hazard assessment, zonation, and earthquake risk mitigation in Armenia.
Title: Probabilistic Seismic Hazard Assessment of Armenia Using an Integrated Seismotectonic Framework
Description:
Armenia is located within the central segment of the Arabia–Eurasia continental collision zone and is exposed to significant seismic hazard.
This study presents an updated probabilistic seismic hazard assessment (PSHA) for Armenia based on an integrated seismotectonic framework incorporating active fault data, paleoseismological evidence, and historical and instrumental seismicity.
A hybrid seismic source model was developed by combining fault-based characteristic earthquake sources with distributed background seismicity.
Hazard calculations were performed using the OpenQuake engine within a logic-tree framework to account for epistemic uncertainties in earthquake occurrence and ground-motion prediction.
Ground motion was estimated using a weighted set of ground motion prediction equations (GMPEs).
Peak ground acceleration (PGA) hazard maps were computed for several return periods, with emphasis on the 475-year return period (10% probability of exceedance in 50 years).
The results indicate PGA values across Armenia ranging from approximately 0.
2 g to 0.
5 g, with the highest hazard levels in northwestern Armenia along the Pambak–Sevan–Syunik Fault System.
Hazard deaggregation shows that seismic hazard in major Armenian cities is primarily controlled by shallow earthquakes with magnitudes Mw 6.
8–7.
4 occurring within ~30 km of urban centers.
The results provide a scientific basis for seismic hazard assessment, zonation, and earthquake risk mitigation in Armenia.
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