Abstract
In the present study, we propose a new approach for determining earthquake hypocentral parameters. This approach integrates computed theoretical seismograms and deep machine learning. The theoretical seismograms are generated through a realistic three-dimensional Earth model, and are then used to create spatial images of seismic wave propagation at the Earth’s surface. These snapshots are subsequently utilized as a training data set for a convolutional neural network. Neural networks for determining hypocentral parameters such as the epicenter, depth, occurrence time, and magnitude are established using the temporal evolution of the snapshots. These networks are applied to seismograms from the seismic observation network in the Hakone volcanic region in Japan to demonstrate the suitability of the proposed approach for locating earthquakes. We demonstrate that the determination accuracy of hypocentral parameters can be improved by including theoretical seismograms for different earthquake locations and sizes, in the learning data set for the deep machine learning. Using the proposed method, the hypocentral parameters are automatically determined within seconds after detecting an event. This method can potentially serve in monitoring earthquake activity in active volcanic areas such as the Hakone region.
Highlights
The machine learning technique is widely exploited in disciplines of science and technology including seismology (Maggi et al 2017; Rouet-Leduc et al 2017; Malfante et al 2018; Nakano et al 2019; Seydoux et al 2020)
Validation and testing for 3DCNN The 600,000 training data images were divided into training data (80%) and validation data (20%)
We demonstrate the application of the proposed technique for accurate and rapid micro earthquake monitoring in the Hakone volcanic region in Japan
Summary
The machine learning technique is widely exploited in disciplines of science and technology including seismology (Maggi et al 2017; Rouet-Leduc et al 2017; Malfante et al 2018; Nakano et al 2019; Seydoux et al 2020). Combining numerical seismograms and pattern recognition for earthquake location was proposed by Käufl et al (2014, 2015, 2016a, b). According to these studies, the technique can be applied for determining fault parameters. The 3D SEM was initially employed in seismology to perform local and regional simulations (Faccioli et al 1997; Komatitsch 1997; Komatitsch and Vilotte 1998), and later adapted for wave propagation at the Earth scale (Komatitsch and Tromp 2002a; b; Komatitsch et al 2005; Tsuboi et al 2003, 2016; Carrington et al 2008; Rietmann et al 2012).
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