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Magnitude correlations in global seismicity.
1Solid State Section and Solid Earth Physics Institute, Physics Department, University of Athens, Panepistimiopolis, Zografos GR-157 84, Athens, Greece. nsarlis@phys.uoa.gr
Global seismicity shows significant magnitude correlations for earthquakes exceeding M(w) 6.5. Natural time analysis reveals these nontrivial earthquake magnitude correlations worldwide.
Area of Science:
- Geophysics
- Seismology
- Complex Systems
Background:
- Understanding earthquake patterns is crucial for seismic hazard assessment.
- The complex nature of seismicity suggests potential underlying correlations.
Purpose of the Study:
- To investigate correlations between earthquake magnitudes globally.
- To apply natural time analysis to worldwide seismicity data.
Main Methods:
- Utilized natural time analysis techniques.
- Analyzed global earthquake catalogs focusing on magnitude data.
Main Results:
- Identified nontrivial magnitude correlations in global seismicity.
- These correlations are evident for earthquakes with magnitudes greater than M(w) 6.5.
Conclusions:
- Global seismicity exhibits statistically significant correlations in earthquake magnitudes above a certain threshold.
- Natural time analysis provides a valuable framework for uncovering hidden patterns in seismic events.
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