Abstract

Strong-motion data from large (M ≥ 7.2) shallow crustal earthquakes invariably make up a small proportion of the records used to develop empirical ground motion prediction equations (GMPEs). Consequently GMPEs are more poorly constrained for large earthquakes than for small events. In this article peak ground accelerations (PGAs) observed in 38 earthquakes worldwide with M ≥ 7.2 are compared with those predicted by eight recent GMPEs. Well over half of the 38 earthquakes were not considered when deriving these GMPEs but the data were identified by a thorough literature review of strong-motion reports from the past 60 years. These data are provided in an electronic supplement for future investigations on ground motions from large earthquakes. The addition of these data provides better constraint of the between-event ground-motion variability in large earthquakes. It is found that the eight models generally provide good predictions for PGAs from these earthquakes, although there is evidence for slight under- or over-prediction of motions by some models (particularly for M > 7.6). The between-event variabilities predicted by most models match the observed variability, if data from two events (2001 Bhuj and 2005 Crescent City) that are likely atypical of earthquakes in active regions are excluded. For some GMPEs there is evidence that they are over-predicting PGAs in the near-source region of large earthquakes as well as over-predicting motions on hard rock. Overall, however, all the considered models, despite having been derived using limited data, provide reliable predictions of PGAs in the largest crustal earthquakes.

Highlights

  • Strong-motion data from large (M C 7.2) shallow crustal earthquakes invariably make up a small proportion of the records used to develop empirical ground motion prediction equations (GMPEs)

  • The maximum distance for which the selected GMPEs are recommended for use by their developers varies between 150 km (Cauzzi et al 2015) and 400 km (Boore et al 2014), with most suggesting 300 km

  • The majority of the GMPEs have an overall bias in their predictions of less than 10%, with the largest bias being less than 20% when data to 400 km are considered

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Summary

Introduction

Given more time this study could obviously be repeated with a lower magnitude limit but it is likely that the conclusions would be similar From this search, 23 earthquakes, in addition to the 15 contained in the NGA-West database, were identified as having PGA observations from ground-response stations (these are not necessarily ‘‘free-field’’ installations—the instrument housing may have slightly affected the measured ground motions). The selected GMPEs all use the average shear-wave velocity in the top 30 m (VS30) to characterise the near-surface site conditions at the strong-motion stations If this information was available in the NGA-West database or was given in other published sources, these estimates are used. An Excel spreadsheet is provided as an Electronic Supplement, which contain the data used for this study and the references

Comparisons to GMPEs
Magnitude scaling
Distance scaling
VS30 scaling
Ground-motion variability
Findings
Conclusions
Full Text
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