Japan Geoscience Union Meeting 2025

Presentation information

[J] Poster

S (Solid Earth Sciences ) » S-TT Technology & Techniques

[S-TT43] Seismic Big Data Analysis Based on the State-of-the-Art of Bayesian Statistics

Mon. May 26, 2025 5:15 PM - 7:15 PM Poster Hall (Exhibition Hall 7&8, Makuhari Messe)

convener:Hiromichi Nagao(Earthquake Research Institute, The University of Tokyo), Aitaro Kato(Earthquake Research Institute, the University of Tokyo), Keisuke Yano(The Institute of Statistical Mathematics), Takahiro Shiina(National Institute of Advanced Industrial Science and Technology)

5:15 PM - 7:15 PM

[STT43-P04] PoViT-UQ : P-wave Polarity and Arrival Time Determination using Vision Transformer with Uncertainty Quantification

*Shinya Katoh1, Hiromichi Nagao1, Yoshihisa Iio2 (1.Earthquake Research Institute,The University of Tokyo, 2.ABUYAMA Seismological MUSEUM)

Keywords:P-wave Polarity, Focal Mechanism, Deep Learning

Determining earthquake focal mechanisms is important. Estimating them using P-wave polarities is often not robust (Hardebeck and Shearer, 2002). Therefore, automating this process requires high-confidence data. In recent years, deep learning-based polarity determination models have been developed (Ross et al., 2018; Hara et al., 2019; Uchide et al., 2020; Zhang et al., 2023). However, previous deep learning models are point estimation models and cannot evaluate confidence levels. In this study, we propose a novel deep learning model, PoViT-UQ, which combines a Vision Transformer (ViT; Dosovitskiy et al., 2021) with Monte Carlo Dropout (MCD; Gal and Ghahramani, 2016) to estimate high-precision initial P-wave polarity classification and arrival time detection with uncertainty quantification. Using seismic waveform data sampled at 100 Hz and 250 Hz, the model classifies polarities into three classes (Up, Down, and Noise) and simultaneously estimates P-wave arrival times. The results show a classification accuracy exceeding 98% and a standard deviation of 0.027 seconds in arrival time estimation with the 250 Hz model. By integrating MCD, we evaluate prediction uncertainty and apply an interquartile range (IQR) threshold of 0.15 or less to improve the accuracy of focal mechanism estimates. Validation using aftershock data from the 2016 Central Tottori Earthquake confirms that our approach contributes to efficient and high-precision focal mechanism estimates. Our model advances automated initial P-wave polarity determination and enables reliable data selection based on uncertainty quantification, significantly improving upon the limitations of conventional models.