1999
DOI: 10.1785/bssa0890051379
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Earthquake hazard in Mexico City: Observations versus computations

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Cited by 67 publications
(8 citation statements)
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“…For moderate intensities, the differences between both hazard curves are not so large and seem t for the observed data. Similar observations were made by (Ordaz and Reyes 1999).…”
Section: Comparison With Previous Modelssupporting
confidence: 89%
“…For moderate intensities, the differences between both hazard curves are not so large and seem t for the observed data. Similar observations were made by (Ordaz and Reyes 1999).…”
Section: Comparison With Previous Modelssupporting
confidence: 89%
“…Düzce is affected by two of the fourteen seismic sources (zones 1 and 2) for Turkey, as described by Erdik et al (1985), Yaltirak et al (1998) and Kayabali and Akin (2002). Seismic hazard analysis of Düzce has been conducted applying a poissonian probabilistic approach, using CRISIS 99 code (Ordaz 1999), for mean return periods of 100, 475 and 1000 years in a grid of 1 km × 1 km for the city of Düzce (Alexoudi 2005). The main assumption for the seismic source used is that earthquakes occur only along faults (Kayabali and Akin 2002).…”
Section: Düzcementioning
confidence: 99%
“…This model includes the earthquake occurrence modeling, magnitude-recurrence relation, seismic source zones, and ground motion prediction equations (GMPEs). The model considers the seismic sources presented in Figure 3, where the seismic sources are separated into three groups (Ordaz and Reyes, 1999;Jaimes and Reinoso, 2006;Reinoso and Jaimes 2009;Nishenko and Singh 1987), depending on the type of earthquake and magnitude considered. The magnitude-recurrence relation and parameters defining the source zones are given by Ordaz and Reyes (1999) for interplate events, and by Jaimes and Reinoso (2006) for intraslab events.…”
Section: Simulation Of the Peak Ground Accelerations And Scaling Of T...mentioning
confidence: 99%
“…The model considers the seismic sources presented in Figure 3, where the seismic sources are separated into three groups (Ordaz and Reyes, 1999;Jaimes and Reinoso, 2006;Reinoso and Jaimes 2009;Nishenko and Singh 1987), depending on the type of earthquake and magnitude considered. The magnitude-recurrence relation and parameters defining the source zones are given by Ordaz and Reyes (1999) for interplate events, and by Jaimes and Reinoso (2006) for intraslab events. The GMPEs employed were those developed by Hong et al (2009) for interplate and intraslab events for places outside Mexico City.…”
Section: Simulation Of the Peak Ground Accelerations And Scaling Of T...mentioning
confidence: 99%