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The ISC Bulletin as a comprehensive source of earthquake source mechanisms
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Abstract. In this article we summarize the availability of earthquake source mechanisms in the Bulletin of the International Seismological Centre (ISC). The bulletin in its current status contains ∼ 81,000 seismic events with only one associated mechanism solution, and ∼ 22,000 events with at least two associated source mechanisms. The main sources of earthquake mechanisms in the ISC Bulletin are reported solutions provided by data contributors, and ISC computed focal mechanisms based on first motion polarities. Given the importance of using pre-determined fault plane solutions in different types of studies, here we focus only on the reported mechanisms and we briefly discuss the methodologies adopted by major data providers to the ISC and investigate the intra-event variability of the source mechanisms. We conclude that the overall agreement among different earthquake focal mechanisms for the same event as reported by different sources can be as high as 90% for the majority of the cases. The earthquake source mechanisms discussed in this work are freely available within the ISC Bulletin websearch at http://doi.org/10.31905/D808B830.
Title: The ISC Bulletin as a comprehensive source of earthquake source mechanisms
Description:
Abstract.
In this article we summarize the availability of earthquake source mechanisms in the Bulletin of the International Seismological Centre (ISC).
The bulletin in its current status contains ∼ 81,000 seismic events with only one associated mechanism solution, and ∼ 22,000 events with at least two associated source mechanisms.
The main sources of earthquake mechanisms in the ISC Bulletin are reported solutions provided by data contributors, and ISC computed focal mechanisms based on first motion polarities.
Given the importance of using pre-determined fault plane solutions in different types of studies, here we focus only on the reported mechanisms and we briefly discuss the methodologies adopted by major data providers to the ISC and investigate the intra-event variability of the source mechanisms.
We conclude that the overall agreement among different earthquake focal mechanisms for the same event as reported by different sources can be as high as 90% for the majority of the cases.
The earthquake source mechanisms discussed in this work are freely available within the ISC Bulletin websearch at http://doi.
org/10.
31905/D808B830.
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