Geodetic Constraints on Segment-Scale Slip Rates and Interseismic Coupling Along the Havran-Balıkesir Fault Zone, NW Anatolia, Türkiye. [PDF]
Tiryakioğlu İ +12 more
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Large-magnitude events unlikely in induced earthquake sequences. [PDF]
Li L, Im K, Avouac JP.
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XGBoost-based ground motion model for constant-strength inelastic acceleration response spectra. [PDF]
Gong Y, Zhao J.
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Updated seismotectonic framework of Abu Dabbab Egypt based on focal mechanisms and stress inversion. [PDF]
Abdelazim M +7 more
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Earthquake Early Warning System for Izmir, Western Anatolia, Türkiye Based on Multi-Station Similarity Analysis and Real-Time Seismic Data Processing. [PDF]
Doğan Y +13 more
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Advanced Seismic Hazard AssessmentPart I: Seismic Hazard Assessment
Seismic Hazard ...
PANZA, GIULIANO +5 more
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A simplified seismotectonic model is proposed for Bulgaria by introducing generalized seismogenic areas containing systems of complex geometry faults. A tectonic scheme, which considers the main faults only, is then derived from this. The assessment of the regional seismic hazard is done using different approaches: the Gumbel, the Cornell, and the ...
Ivanka Orozova-Stanishkova, Dario Slejko
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Seismicity, seismotectonics and seismic hazard of Italy
Engineering Geology, 2000Abstract A first generation of probabilistic seismic hazard maps of the Italian country are presented. They are based on seismogenic zoning deriving from a kinematic model of the structural tectonic units and on an earthquake catalogue with the foreshock and aftershock events filtered out. The following ground motion parameters have been investigated
ROMEO, ROBERTO, PUGLIESE A.
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A textbook designed for students taking a course in Natural Hazards with an Australasian focus and context. Full colour and richly supported by photographs, illustrations and maps.
Quigley, MC, Duffy, B
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Origin of Seismicity in Italy as a Clue for Seismic Hazard
2023Italian seismicity is generated by the ongoing subduction of the European lithosphere beneath the Alps, and the Adriatic lithosphere beneath the Apennines. The two belts are extremely different due to their opposite polarity relative to the inferred underlying ‘eastward’ mantle flow.
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