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Predicting fault slip via transfer learning
Kun Wang1,2, Christopher W Johnson1, Kane C Bennett1
1Geophysics Group, Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM, 87545, USA.
Nature Communications
|December 17, 2021
Summary
Transfer learning with simulations accurately predicts laboratory fault slip. Fine-tuning with limited earthquake data further improves predictions, showing potential for real-world fault behavior forecasting.
Area of Science:
- Geophysics
- Machine Learning
- Computational Seismology
Background:
- Machine learning models for predicting fault slip show promise but require extensive training data.
- Earthquake data is sparse, posing a significant challenge for training predictive models for real-world fault behavior.
Purpose of the Study:
- To develop a transfer learning approach for predicting fault slip using numerical simulations.
- To investigate the efficacy of training a convolutional encoder-decoder model with simulated data and fine-tuning it with laboratory experimental data.
Main Methods:
- A convolutional encoder-decoder model was trained using acoustic emission and fault friction data from numerical simulations.
- The trained model was then applied to predict fault-slip behavior in laboratory experiments.
- Further fine-tuning of the model's latent space was performed using limited data from a single laboratory earthquake cycle.
Main Results:
- The transfer learning model accurately predicted fault friction in laboratory experiments.
- Fine-tuning the model with a small subset of laboratory data significantly improved prediction accuracy.
- The study demonstrates successful generalization from simulated to experimental data.
Conclusions:
- Transfer learning offers a viable solution for training machine learning models on sparse geophysical data.
- Models trained on numerical simulations can be effectively adapted for predicting fault slip in laboratory settings.
- This approach holds potential for improving earthquake forecasting and understanding fault behavior in Earth.
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