A deep-learning-based approach for seismic surface-wave dispersion inversion (SfNet) with application to the Chinese mainland

IF 1.2 4区 地球科学 Q3 Earth and Planetary Sciences
Feiyi Wang , Xiaodong Song , Mengkui Li
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引用次数: 1

Abstract

Surface-wave tomography is an important and widely used method for imaging the crust and upper mantle velocity structure of the Earth. In this study, we proposed a deep learning (DL) method based on convolutional neural network (CNN), named SfNet, to derive the vS model from the Rayleigh wave phase and group velocity dispersion curves. Training a network model usually requires large amount of training datasets, which is labor-intensive and expensive to acquire. Here we relied on synthetics generated automatically from various spline-based vS models instead of directly using the existing vS models of an area to build the training dataset, which enhances the generalization of the DL method. In addition, we used a random sampling strategy of the dispersion periods in the training dataset, which alleviates the problem that the real data used must be sampled strictly according to the periods of training dataset. Tests using synthetic data demonstrate that the proposed method is much faster, and the results for the vS model are more accurate and robust than those of conventional methods. We applied our method to a dataset for the Chinese mainland and obtained a new reference velocity model of the Chinese continent (ChinaVs-DL1.0), which has smaller dispersion misfits than those from the traditional method. The high accuracy and efficiency of our DL approach makes it an important method for vS model inversions from large amounts of surface-wave dispersion data.

基于深度学习的地震表面波频散反演方法及其在中国大陆的应用
表面波层析成像是一种重要的、广泛应用的地球地壳和上地幔速度结构成像方法。在这项研究中,我们提出了一种基于卷积神经网络(CNN)的深度学习(DL)方法,命名为SfNet,从瑞利波相位和群速度色散曲线中导出vS模型。训练网络模型通常需要大量的训练数据集,这是一项劳动密集型的工作,并且获取成本昂贵。在这里,我们依赖于各种基于样条的vS模型自动生成的合成,而不是直接使用一个区域的现有vS模型来构建训练数据集,这增强了DL方法的泛化性。此外,我们在训练数据集中采用了离散周期的随机采样策略,缓解了实际使用的数据必须严格按照训练数据集的周期进行采样的问题。利用综合数据进行的测试表明,该方法的速度更快,并且vS模型的结果比传统方法更准确和鲁棒。将该方法应用于中国大陆数据集,得到了一个新的中国大陆参考速度模型(ChinaVs-DL1.0),该模型比传统方法具有更小的频散错拟合。该方法的高精度和高效率使其成为从大量表面波色散数据反演vS模型的重要方法。
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来源期刊
Earthquake Science
Earthquake Science GEOCHEMISTRY & GEOPHYSICS-
CiteScore
1.10
自引率
8.30%
发文量
42
审稿时长
3 months
期刊介绍: Earthquake Science (EQS) aims to publish high-quality, original, peer-reviewed articles on earthquake-related research subjects. It is an English international journal sponsored by the Seismological Society of China and the Institute of Geophysics, China Earthquake Administration. The topics include, but not limited to, the following ● Seismic sources of all kinds. ● Earth structure at all scales. ● Seismotectonics. ● New methods and theoretical seismology. ● Strong ground motion. ● Seismic phenomena of all kinds. ● Seismic hazards, earthquake forecasting and prediction. ● Seismic instrumentation. ● Significant recent or past seismic events. ● Documentation of recent seismic events or important observations. ● Descriptions of field deployments, new methods, and available software tools. The types of manuscripts include the following. There is no length requirement, except for the Short Notes. 【Articles】 Original contributions that have not been published elsewhere. 【Short Notes】 Short papers of recent events or topics that warrant rapid peer reviews and publications. Limited to 4 publication pages. 【Rapid Communications】 Significant contributions that warrant rapid peer reviews and publications. 【Review Articles】Review articles are by invitation only. Please contact the editorial office and editors for possible proposals. 【Toolboxes】 Descriptions of novel numerical methods and associated computer codes. 【Data Products】 Documentation of datasets of various kinds that are interested to the community and available for open access (field data, processed data, synthetic data, or models). 【Opinions】Views on important topics and future directions in earthquake science. 【Comments and Replies】Commentaries on a recently published EQS paper is welcome. The authors of the paper commented will be invited to reply. Both the Comment and the Reply are subject to peer review.
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