利用先进的机器学习算法进行哥伦比亚地震监测

Emmanuel Castillo, Daniel Siervo, G. Prieto
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引用次数: 0

摘要

全球地震网络旨在监测地震地面运动。这一过程包括识别信号中的地震事件、挑选和关联地震相位、确定事件位置以及计算震级。虽然机器学习(ML)方法在其中一些步骤上有了显著的改进,但在其他一些阶段,传统的非 ML 算法也优于 ML 方法。我们介绍的 SeisMonitor 是一款用于监测地震活动的 Python 开源软件包,它使用现成的 ML 方法进行事件检测、相位选择和关联,并在其余步骤中使用其他众所周知的方法。我们在哥伦比亚境内的三个地震网络(哥伦比亚地震网络和南美洲北部的两个本地临时网络:中马格达莱纳河谷和加勒比海-梅里达安第斯地震阵列)中应用了这些步骤,整个过程完全自动化,历时近 7 年(2016-2022 年)。研究结果表明,这种方法在创建自动地震目录方面非常可靠,其地震探测能力和定位精度与标准目录类似。此外,它还能有效识别重要的构造结构,并强调局部地壳断层。此外,该方法还具有提高地震处理效率的潜力,并且由于其检测小震和余震的能力,可作为人工地震目录的重要补充。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Colombian Seismic Monitoring Using Advanced Machine-Learning Algorithms
Seismic networks worldwide are designed to monitor seismic ground motion. This process includes identifying seismic events in the signals, picking and associating seismic phases, determining the event’s location, and calculating its magnitude. Although machine-learning (ML) methods have shown significant improvements in some of these steps individually, there are other stages in which traditional non-ML algorithms outperform ML approaches. We introduce SeisMonitor, a Python open-source package to monitor seismic activity that uses ready-made ML methods for event detection, phase picking and association, and other well-known methods for the rest of the steps. We apply these steps in a totally automated process for almost 7 yr (2016–2022) in three seismic networks located in Colombian territory, the Colombian seismic network and two local and temporary networks in northern South America: the Middle Magdalena Valley and the Caribbean-Mérida Andes seismic arrays. The results demonstrate the reliability of this method in creating automated seismic catalogs, showcasing earthquake detection capabilities and location accuracy similar to standard catalogs. Furthermore, it effectively identifies significant tectonic structures and emphasizes local crustal faults. In addition, it has the potential to enhance earthquake processing efficiency and serve as a valuable supplement to manual catalogs, given its ability at detecting minor earthquakes and aftershocks.
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