论文标题

与神经操作员进行实时地震位置的加速时间反转成像

Accelerating Time-Reversal Imaging with Neural Operators for Real-time Earthquake Locations

论文作者

Sun, Hongyu, Yang, Yan, Azizzadenesheli, Kamyar, Clayton, Robert W., Ross, Zachary E.

论文摘要

地震低中心构成了广泛的地震学分析的基础。基于采摘的地震位置工作流程依赖相拾取器的准确性,在处理异质介质中复杂的地震序列时可能会偏差。具有互相关成像条件的被动地震源的时间反转成像具有高精度和高分辨率的地震位置的潜力,但具有较大的计算成本。在这里,我们通过将神经操作员的益处与多站波形记录相结合,为地震位置提供了一种替代性深度学习方法。对U形神经操作员进行了训练,可以通过各种源时间函数传播地震波,因此可以预测每个站点可忽略不计的反向传播波场。这些波场可以堆叠或相关,以从所得的源图像中找到地震。与其他基于波形的深度学习位置方法相比,时间逆转成像解释了波传播的物理定律,并有望实现准确的地震位置。我们在合成数据和场数据上都用2D声波方程来演示该方法。结果表明,我们的方法可以有效地获得地震来源的高分辨率和高精度基于相关性的时间反转成像。此外,我们的方法适应地震站的数量和几何形状,该地震站为实时地震位置打开了新的策略,并通过密集的地震网络进行监测。

Earthquake hypocenters form the basis for a wide array of seismological analyses. Pick-based earthquake location workflows rely on the accuracy of phase pickers and may be biased when dealing with complex earthquake sequences in heterogeneous media. Time-reversal imaging of passive seismic sources with the cross-correlation imaging condition has potential for earthquake location with high accuracy and high resolution, but carries a large computational cost. Here we present an alternative deep-learning approach for earthquake location by combining the benefits of neural operators for wave propagation and time reversal imaging with multi-station waveform recordings. A U-shaped neural operator is trained to propagate seismic waves with various source time functions and thus can predict a backpropagated wavefield for each station in negligible time. These wavefields can either be stacked or correlated to locate earthquakes from the resulting source images. Compared with other waveform-based deep-learning location methods, time reversal imaging accounts for physical laws of wave propagation and is expected to achieve accurate earthquake location. We demonstrate the method with the 2D acoustic wave equation on both synthetic and field data. The results show that our method can efficiently obtain high resolution and high accuracy correlation-based time reversal imaging of earthquake sources. Moreover, our approach is adaptable to the number and geometry of seismic stations, which opens new strategies for real-time earthquake location and monitoring with dense seismic networks.

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