An envelope-based machine learning workflow for locating earthquakes in the southern Sichuan Basin

Kang Wang, Jie Zhang, Ji Zhang, Zhangyu Wang, Ziyu Li
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Abstract

The development of machine learning technology enables more robust real-time earthquake monitoring through automated implementations. However, the application of machine learning to earthquake location problems faces challenges in regions with limited available training data. To address the issues of sparse event distribution and inaccurate ground truth in historical seismic datasets, we expand the training dataset by using a large number of synthetic envelopes that closely resemble real data and build an earthquake location model named ENVloc. We propose an envelope-based machine learning workflow for simultaneously determining earthquake location and origin time. The method eliminates the need for phase picking and avoids the accumulation of location errors resulting from inaccurate picking results. In practical application, ENVloc is applied to several data intercepted at different starting points. We take the starting point of the time window corresponding to the highest prediction probability value as the origin time and save the predicted result as the earthquake location. We apply ENVloc to observed data acquired in the southern Sichuan Basin, China, between September 2018 and March 2019. The results show that the average difference with the catalog in latitude, longitude, depth, and origin time is 0.02°, 0.02°, 2 ​km, and 1.25 ​s, respectively. These suggest that our envelope-based method provides an efficient and robust way to locate earthquakes without phase picking, and can be used in earthquake monitoring in near-real time.

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四川盆地南部地震定位的基于包络的机器学习工作流程
机器学习技术的发展通过自动实施实现了更强大的实时地震监测。然而,在可用训练数据有限的地区,将机器学习应用于地震定位问题面临挑战。为了解决历史地震数据集中事件分布稀疏和地面实况不准确的问题,我们使用大量与真实数据非常相似的合成包络来扩展训练数据集,并建立了名为 ENVloc 的地震定位模型。我们提出了一种基于包络的机器学习工作流程,用于同时确定地震位置和起源时间。该方法无需进行相位选取,避免了因选取结果不准确而导致的位置误差累积。在实际应用中,ENVloc 适用于在不同起点截取的多个数据。我们将预测概率值最高的时间窗对应的起点作为原点时间,并将预测结果保存为地震位置。我们将 ENVloc 应用于 2018 年 9 月至 2019 年 3 月期间在中国四川盆地南部获取的观测数据。结果表明,在纬度、经度、深度和起源时间上与目录的平均差异分别为 0.02°、0.02°、2 km 和 1.25 s。这表明,我们基于包络的方法提供了一种无需相位选取的高效、稳健的地震定位方法,可用于近实时地震监测。
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