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Spatiotemporal Graph Convolutional Networks for Earthquake Source Characterization
Xitong Zhang1,2, Will Reichard-Flynn1, Miao Zhang3
1Geophysics Group Earth and Environmental Sciences Division Los Alamos National Laboratory Los Alamos NM USA.
Summary
A new Spatiotemporal Graph Neural Network (STGNN) improves earthquake epicenter location accuracy by utilizing data from multiple seismic stations. This deep learning approach enhances seismic data analysis for better earthquake characterization.
Area of Science:
- Seismology
- Geophysics
- Artificial Intelligence
Background:
- Accurate earthquake location and magnitude are crucial in seismology.
- Deep learning shows promise in seismological tasks, but many methods use single-station data.
- Multiple seismic stations offer more comprehensive information for source characterization.
Purpose of the Study:
- To develop a Spatiotemporal Graph Neural Network (STGNN) for improved earthquake location and magnitude estimation.
- To leverage geographical and waveform data from multiple stations for enhanced earthquake analysis.
- To compare STGNN performance against existing deep learning models.
Main Methods:
- Developed a Spatiotemporal Graph Neural Network (STGNN) that uses multi-station seismic data.
- Constructed dynamic graphs using geographical and waveform information with adaptive message passing.
- Applied STGNN to earthquake data from the Southern California Seismic Network and Oklahoma.
Main Results:
- STGNN achieved more accurate earthquake epicenter locations compared to baseline models.
- Depth and magnitude prediction performance was comparable to baselines, indicating a general challenge for all tested models.
- The study demonstrated the effectiveness of GNNs in analyzing multi-station seismic data.
Conclusions:
- Spatiotemporal Graph Neural Networks show significant potential for improving automatic earthquake epicenter estimation.
- Utilizing data from multiple seismic stations within a GNN framework enhances earthquake source characterization.
- Further research is needed to improve depth and magnitude prediction accuracy in seismic event analysis.

