Source scaling comparison and validation in Central Italy: data intensive direct S waves versus the sparse data coda envelope methodology

Robustness of source parameter estimates is a fundamental issue in understanding the relationships between small and large events; however, it is difficult to assess how much of the variability of the source parameters can be attributed to the physical source characteristics or to the uncertainties...

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Veröffentlicht in:Geophysical journal international 2022-09, Vol.231 (3), p.1573-1590
Hauptverfasser: Morasca, Paola, Bindi, Dino, Mayeda, Kevin, Roman-Nieves, Jorge, Barno, Justin, Walter, William R, Spallarossa, Daniele
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Sprache:eng
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Zusammenfassung:Robustness of source parameter estimates is a fundamental issue in understanding the relationships between small and large events; however, it is difficult to assess how much of the variability of the source parameters can be attributed to the physical source characteristics or to the uncertainties of the methods and data used to estimate the values. In this study, we apply the coda method by Mayeda et al. using the coda calibration tool (CCT), a freely available Java-based code (https://github.com/LLNL/coda-calibration-tool) to obtain a regional calibration for Central Italy for estimating stable source parameters. We demonstrate the power of the coda technique in this region and show that it provides the same robustness in source parameter estimation as a data-driven methodology [generalized inversion technique (GIT)], but with much fewer calibration events and stations. The Central Italy region is ideal for both GIT and coda approaches as it is characterized by high-quality data, including recent well-recorded seismic sequences such as L'Aquila (2009) and Amatrice–Norcia–Visso (2016–2017). This allows us to apply data-driven methods such as GIT and coda-based methods that require few, but high-quality data. The data set for GIT analysis includes ∼5000 earthquakes and more than 600 stations, while for coda analysis we used a small subset of 39 events spanning 3.5 
ISSN:0956-540X
1365-246X
DOI:10.1093/gji/ggac268