High-rate phase association with travel time neural fields.
Cheng Shi1,2, Giulio Poggiali3, Chris Marone3,4
1Department of Mathematics and Computer Science, University of Basel, Basel, Switzerland.
A new framework, HARPA, improves earthquake phase association by using optimal transport and neural networks to model wave speeds. This method enhances the analysis of dense seismic data, especially in complex geological areas.
Area of Science:
- Earthquake science
- Seismology
- Geophysics
Background:
- Phase association is crucial for grouping seismic arrivals to identify earthquake sources.
- Deep learning has increased the detection rate of small seismic events, leading to high-rate arrival sequences.
- Associating these dense seismic data is challenging, particularly with heterogeneous or unknown wave speeds.
Purpose of the Study:
- To introduce HARPA, a novel phase-association framework.
- To improve the association of seismic arrivals in dense and complex scenarios.
- To jointly estimate earthquake parameters and wave-speed fields.
Main Methods:
- HARPA utilizes optimal transport metrics to compare probability distributions of observed and predicted arrival sequences.
- It employs travel-time neural fields (neural networks) to model wave speeds and estimate earthquake locations and origin times.
- The framework handles high-rate arrival sequences and heterogeneous wave-speed fields.
Main Results:
- HARPA performs comparably to state-of-the-art methods on standard, low-rate datasets with simple wave speeds.
- It outperforms existing methods significantly at high seismic event rates and with laterally heterogeneous or unknown wave speeds.
- The study highlights the importance of adaptive travel-time modeling for dense seismicity.
Conclusions:
- HARPA offers a robust solution for phase association, especially in challenging environments with dense seismicity.
- The framework's ability to jointly model wave speeds advances seismic data analysis.
- This work suggests a pathway for integrating phase association with passive-source tomography.
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