EQGraphNet:通过具有残差连接的深度图网络推进单站地震震级估算

Zhiguo Wang , Ziwei Chen , Huai Zhang
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引用次数: 0

摘要

震级估计是地震学中的一项关键任务,传统方法通常需要密集的地震台阵列来提供具有足够时空分布的数据。在这种情况下,我们提出了地震图网络(EQGraphNet)来提高单台站震级估计的性能。该模型的骨干由 11 个卷积神经网络层和 10 个 RCGL 模块组成,其中 RCGL 结合了残差连接和图卷积层,能够缓解过度平滑问题,同时提取地震信号的时间特征。我们的工作使用斯坦福大学地震数据集进行模型训练和性能测试。与现有的三个深度学习模型相比,EQGraphNet 在局部震级和持续时间震级尺度上的准确性都有所提高。为了评估鲁棒性,我们在模型输入中添加了自然背景噪声,结果发现 EQGraphNet 取得了最佳结果,尤其是对于信噪比较低的信号。此外,通过替换各种网络组件并比较其估计性能,我们说明了 EQGraphNet 各部分的贡献,验证了我们方法的合理性。我们还证明了我们的模型在不同地震发生环境下的泛化能力,其平均误差为 ±0.1 个单位。此外,通过证明更深层架构的有效性,这项工作鼓励进一步探索用于多站和单站震级估计的更深层 GNN 模型。
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EQGraphNet: Advancing single-station earthquake magnitude estimation via deep graph networks with residual connections

Magnitude estimation is a critical task in seismology, and conventional methods usually require dense seismic station arrays to provide data with sufficient spatiotemporal distribution. In this context, we propose the Earthquake Graph Network (EQGraphNet) to enhance the performance of single-station magnitude estimation. The backbone of the proposed model consists of eleven convolutional neural network layers and ten RCGL modules, where a RCGL combines a Residual Connection and a Graph convolutional Layer capable of mitigating the over-smoothing problem and simultaneously extracting temporal features of seismic signals. Our work uses the STanford EArthquake Dataset for model training and performance testing. Compared with three existing deep learning models, EQGraphNet demonstrates improved accuracy for both local magnitude and duration magnitude scales. To evaluate the robustness, we add natural background noise to the model input and find that EQGraphNet achieves the best results, particularly for signals with lower signal-to-noise ratios. Additionally, by replacing various network components and comparing their estimation performances, we illustrate the contribution of each part of EQGraphNet, validating the rationality of our approach. We also demonstrate the generalization capability of our model across different earthquakes occurring environments, achieving mean errors of ±0.1 units. Furthermore, by demonstrating the effectiveness of deeper architectures, this work encourages further exploration of deeper GNN models for both multi-station and single-station magnitude estimation.

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