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Synthetic records are generated by using a stochastic finite-fault model coupled with a long period pulse to capture the long period fling effect.
Synthetic records of 6 April 2009 L′Aquila (Italy) earthquake (Mw=6.3) are simulated using both the Hybrid Integral-Composite method and the Stochastic Finite-Fault method.
Before using the seismologically acceptable synthetic records for engineering purposes, it is critical to investigate the efficiency of synthetics in predicting observed seismic responses of structures.
This method has been shown applicable under synthetic records, too.
Even these supposedly synthetic records can closely match real ones (especially when the underlying aggregate sample is small).
To deal with the uncertainty in the geological records, Huybers developed a methodology through tinkering with "synthetic" records.
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Frieda, K. L. et al. Synthetic recording and in situ readout of lineage information in single cells.
Fig. 2 Observed and synthetic record sections.
Fig. 8 Observed and synthetic record section for OBS026 on ECr25.
Like the synthetic record, the palaeorecord contained a much higher frequency of extreme events than the historical record.
Another example of the record section at OBS063 is shown in Fig. 6(a), which shows a reasonably good consistency both in travel times and amplitudes of the signals between the observed and synthetic record sections (Fig. 6(b)).
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