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Verifying the Magnitude Dependence in Earthquake Occurrence
Giuseppe Petrillo1, Jiancang Zhuang1
1The Institute of Statistical Mathematics, Research Organization of Information and Systems, 10-3 Midoricho, Tachikawa, Tokyo 190-0014, Japan.
Magnitude dependence in earthquake triggering is debated. This study rejects the magnitude correlation hypothesis using synthetic and real earthquake data, suggesting it
Area of Science:
- Seismology
- Earthquake Science
- Geophysics
Background:
- Magnitude dependence in earthquake triggering has been reported, impacting seismic predictability.
- The cause of this correlation is debated, with possibilities including physical processes or data incompleteness (missing short-term aftershocks).
Purpose of the Study:
- To investigate and resolve the debate surrounding magnitude dependence in earthquake triggering.
- To determine if a correlation between earthquake magnitudes is a physical phenomenon or an artifact of incomplete seismic catalogs.
Main Methods:
- Analysis of a synthetic earthquake catalog generated by a numerical model simulating earthquake statistics.
- Application of the stochastic declustering method to a high-resolution earthquake catalog of the Amatrice-Norcia (2016) sequence.
- Focusing analysis on events above the determined magnitude of completeness to ensure data reliability.
Main Results:
- The study found no statistically significant evidence to support a magnitude correlation in earthquake triggering.
- Analysis of both synthetic and real-world earthquake data led to the rejection of the magnitude correlation hypothesis.
Conclusions:
- The observed magnitude dependence in earthquake triggering is likely not a physical characteristic of seismic processes.
- Data incompleteness, particularly the omission of short-term aftershocks, may explain previous reports of magnitude correlation.
- This finding has implications for understanding earthquake predictability and catalog completeness.
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