Ensemble Smoothed Seismicity Models for the New Italian Probabilistic Seismic Hazard Map

2018 ◽  
Vol 89 (4) ◽  
pp. 1277-1287 ◽  
Author(s):  
Aybige Akinci ◽  
Morgan P. Moschetti ◽  
Matteo Taroni
Keyword(s):  
Seismic Hazard ◽  
Probabilistic Seismic Hazard ◽  
Hazard Map ◽  
Seismicity Models ◽  
Smoothed Seismicity ◽  
Seismic Hazard Map

A probabilistic seismic hazard map for the metropolitan France

2020 ◽  
Vol 18 (5) ◽  
pp. 1865-1898 ◽  
Author(s):  
Stéphane Drouet ◽  
Gabriele Ameri ◽  
Kristell Le Dortz ◽  
Ramon Secanell ◽  
Gloria Senfaute
Keyword(s):  
Seismic Hazard ◽  
Probabilistic Seismic Hazard ◽  
Hazard Map ◽  
Seismic Hazard Map

Seismic Hazard Map for Cuba and Adjacent Areas Using the Spatially Smoothed Seismicity Approach

2008 ◽  
Vol 12 (2) ◽  
pp. 173-196 ◽  
Author(s):  
Julio Garcia ◽  
Dario Slejko ◽  
Alessandro Rebez ◽  
Marco Santulin ◽  
Leonardo Alvarez
Keyword(s):  
Seismic Hazard ◽  
Hazard Map ◽  
Spatially Smoothed Seismicity ◽  
Smoothed Seismicity ◽  
Seismic Hazard Map

scholarly journals Probabilistic seismic hazard map for Bulgaria as a basis for a new building code

2006 ◽  
Vol 6 (6) ◽  
pp. 881-887 ◽  
Author(s):  
S. D. Simeonova ◽  
D. E. Solakov ◽  
G. Leydecker ◽  
H. Busche ◽  
T. Schmitt ◽  
...  
Keyword(s):  
Seismic Hazard ◽  
Attenuation Factor ◽  
Seismic Hazard Assessment ◽  
Building Code ◽  
Probabilistic Seismic Hazard Assessment ◽  
Eurocode 8 ◽  
Probabilistic Seismic Hazard ◽  
Hazard Map ◽  
Intermediate Depth ◽  
Seismic Hazard Map

Abstract. A seismic hazard map proposed as part of a new building code for Bulgaria is presented here on basis of the recommendations in EUROCODE 8. Seismic source zones within an area of about 200 km around Bulgaria were constructed considering seismicity, neotectonic and geological development. The most time consuming work was to establish a homogeneous earthquake catalogue out of different catalogues. The probabilistic seismic hazard assessment in terms of intensities is performed following Cornell (1968) with the program EQRISK (see McGuire, 1976), modified by us for use of intensities. To cope with the irregular isoseismals of the Vrancea intermediate depth earthquakes a special attenuation factor is introduced (Ardeleanu et al., 2005), using detailed macroseismic maps of three major earthquakes. The final seismic hazard is the combination of both contributions, of zones with crustal earthquakes and of the Vrancea intermediate depth earthquakes zone. Calculations are done for recurrence periods of 95, 475 and 10 000 years.

Probabilistic seismic hazard map of Papua New Guinea

2016 ◽  
Vol 81 (2) ◽  
pp. 1003-1025 ◽  
Author(s):  
Hadi Ghasemi ◽  
Chris McKee ◽  
Mark Leonard ◽  
Phil Cummins ◽  
Mathew Moihoi ◽  
...  
Keyword(s):  
Seismic Hazard ◽  
Papua New Guinea ◽  
New Guinea ◽  
Probabilistic Seismic Hazard ◽  
Hazard Map ◽  
Seismic Hazard Map

scholarly journals Probabilistic seismic hazard map for Romania as a basis for a new building code

2005 ◽  
Vol 5 (5) ◽  
pp. 679-684 ◽  
Author(s):  
L. Ardeleanu ◽  
G. Leydecker ◽  
K.-P. Bonjer ◽  
H. Busche ◽  
D. Kaiser ◽  
...  
Keyword(s):  
Seismic Hazard ◽  
Grid Point ◽  
Building Code ◽  
Probabilistic Seismic Hazard Assessment ◽  
Eurocode 8 ◽  
Probabilistic Seismic Hazard ◽  
Hazard Map ◽  
Intermediate Depth ◽  
Attenuation Law ◽  
Seismic Hazard Map

Abstract. A seismic hazard map proposed as part of a new building code for Romania is presented here on basis of the recommendations in EUROCODE 8. Seismic source zones within an area of about 200 km around Romania were constructed considering seismicity, neotectonics and geological development. The probabilistic seismic hazard assessment in terms of intensities is performed following Cornell (1968) with the program EQRISK (see Mc Guire, 1976), modified by us for use of intensities. To cope with the irregular isoseismals of the Vrancea intermediate depth earthquakes a factor Ω is introduced to the attenuation law (Kövesligethy, 1907). Using detailed macroseismic maps of three earthquakes Ω is calculated by fitting the attenuation law to observed intensities, i.e. to local ground conditions. Strong local variation of Ω is avoided by a gridding of 0.5° in longitude and 0.25° in latitude. The contribution of the Vrancea intermediate depth zone to the seismic hazard at each grid point is computed with the corresponding representative Ω. A seismogenic depth of 120 km is assumed. The final seismic hazard is the combination of both contributions, of zones with crustal earthquakes and of the Vrancea intermediate depth earthquakes zone. Calculations are done for a recurrence period of 95, 475 and 10000 years. All maps show the dominating effects of the intermediate depth earthquakes in the Vrancea zone, also for the capital Bucharest.  

scholarly journals Correction to: A probabilistic seismic hazard map for the metropolitan France

2020 ◽  
Vol 18 (9) ◽  
pp. 4543-4545
Author(s):  
Stéphane Drouet ◽  
Gabriele Ameri ◽  
Kristell Le Dortz ◽  
Ramon Secanell ◽  
Gloria Senfaute
Keyword(s):  
Seismic Hazard ◽  
Probabilistic Seismic Hazard ◽  
Hazard Map ◽  
Seismic Hazard Map
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