基于一维深度残差神经网络的小震级地震相位识别研究

Wei Li , Megha Chakraborty , Yu Sha , Kai Zhou , Johannes Faber , Georg Rümpker , Horst Stöcker , Nishtha Srivastava
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引用次数: 5

摘要

可靠的地震相位识别通常具有挑战性,特别是在低震级事件或低信噪比的情况下。随着地震仪的改进和更好的全球覆盖,记录的地震数据量急剧增加。这使得使用传统方法处理地震数据变得非常困难,因此需要更强大、更可靠的方法。在这项研究中,我们开发了一维深度残差神经网络(ResNet)来解决地震信号检测和相位识别问题。该方法在南加州地震台网记录的数据集上进行了训练和测试。结果表明,该方法对地震信号的检测和地震相位的识别具有较好的鲁棒性。与先前提出的深度学习方法相比,所引入的框架在南加州地震数据中心记录的数据集上的地震检测性能提高了约4%,在地震相位识别方面的性能略好。在斯坦福地震数据集上进一步验证了模型的可泛化性。此外,在斯坦福地震数据集的同一子集上,当被不同噪声水平掩盖时,实验结果表明该模型在识别小震级地震相位方面具有鲁棒性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A study on small magnitude seismic phase identification using 1D deep residual neural network

Reliable seismic phase identification is often challenging especially in the circumstances of low-magnitude events or poor signal-to-noise ratio. With improved seismometers and better global coverage, a sharp increase in the volume of recorded seismic data has been achieved. This makes handling seismic data rather daunting by using traditional approaches and therefore fuels the need for more robust and reliable methods. In this study, we develop 1D deep Residual Neural Network (ResNet), for tackling the problem of seismic signal detection and phase identification. This method is trained and tested on the dataset recorded by the Southern California Seismic Network. Results demonstrate that the proposed method can achieve robust performance for the detection of seismic signals and the identification of seismic phases. Compared to previously proposed deep learning methods, the introduced framework achieves around 4% improvement in earthquake detection and a slightly better performance in seismic phase identification on the dataset recorded by Southern California Earthquake Data Center. The model generalizability is also tested further on the STanford EArthquake Dataset. In addition, the experimental result on the same subset of the STanford EArthquake Dataset, when masked by different noise levels, demonstrates the model’s robustness in identifying the seismic phases of small magnitude.

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