低频地震复发的隐马尔可夫模型

Jessica Allen, Ting Wang
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引用次数: 0

摘要

摘要低频地震是频率在1 ~ 10赫兹之间的小震级地震,通常发生在重叠序列中,形成持续性地震。它们提供了对沿板块边界的大地震过程的见解。生命周期在时间上是随机发生的,经常形成时间上反复出现的簇。发生时间通常使用点过程及其强度函数建模。我们演示了如何使用隐马尔可夫模型和可视化技术来直接模拟到达时间,对圣安地列斯断层的LFE发生模式进行分类,并进行模型选择。我们强调了生命周期活动的两个子系统对应于交替发作和静止行为的周期。关键词:分类模型选择圣安德烈亚斯断层可视化viterbi路径免责声明作为对作者和研究人员的服务,我们提供此版本的已接受稿件(AM)。在最终出版版本记录(VoR)之前,将对该手稿进行编辑、排版和审查。在制作和印前,可能会发现可能影响内容的错误,所有适用于期刊的法律免责声明也与这些版本有关。作者希望感谢Jodie Buckby分享拟合和优化隐马尔可夫模型的代码,并提供一般帮助。我们感谢Marco Brenna对地质解释、可视化和其他编辑的建议。作者还希望感谢使用新西兰eScience Infrastructure (NeSI)高性能计算设备和咨询支持作为本研究的一部分。新西兰的国家设施由NeSI提供,由NeSI的合作机构联合资助,并通过商业、创新和就业部的研究基础设施项目。URL https://www.nesi.org.nz。作者感谢两位匿名审稿人对本文的改进建议。补充材料包含(i)用于分析的R代码,(ii)第4.1节中伽玛、威布尔、对数正态和正态隐马尔可夫模型的结果表,(iii)第4.1节中附加的伪残差图和停留检查,(iv)第4.3节中附加的概率密度图和状态分裂序列图,(v)第4.4节中整个观察期和2005年、2006年和2007年的Viterbi路径可视化。(vi)第4.5节中子系统的逗留检查。披露声明作者报告无竞争利益需要申报。
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Hidden Markov Models for Low-Frequency Earthquake Recurrence
AbstractLow-frequency earthquakes (LFEs) are small magnitude earthquakes with frequencies of 1-10 Hertz which often occur in overlapping sequence forming persistent seismic tremors. They provide insights into large earthquake processes along plate boundaries. LFEs occur stochastically in time, often forming temporally recurring clusters. The occurrence times are typically modeled using point processes and their intensity functions. We demonstrate how to use hidden Markov models coupled with visualization techniques to model inter-arrival times directly, classify LFE occurrence patterns along the San Andreas Fault, and perform model selection. We highlight two subsystems of LFE activity corresponding to periods of alternating episodic and quiescent behavior.Keywords: Classificationmodel selectionSan Andreas FaultvisualizationViterbi pathDisclaimerAs a service to authors and researchers we are providing this version of an accepted manuscript (AM). Copyediting, typesetting, and review of the resulting proofs will be undertaken on this manuscript before final publication of the Version of Record (VoR). During production and pre-press, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal relate to these versions also. AcknowledgmentsThe authors wish to thank Jodie Buckby for sharing code to fit and optimize hidden Markov models, and providing general assistance. We are grateful to Marco Brenna for advice regarding geological interpretations, visualization, and additional edits. The authors also wish to acknowledge the use of New Zealand eScience Infrastructure (NeSI) high performance computing facilities and consulting support as part of this research. New Zealand’s national facilities are provided by NeSI and funded jointly by NeSI’s collaborator institutions and through the Ministry of Business, Innovation & Employment’s Research Infrastructure program. URL https://www.nesi.org.nz. The authors acknowledge the suggestions of two anonymous reviewers in enhancing this paper.Supplementary MaterialsThe Supplementary Material contains (i) R code used for the analysis, (ii) tables of results for gamma, Weibull, log-normal and normal hidden Markov models in Section 4.1, (iii) additional pseudo-residual plots and sojourn checks for Section 4.1, (iv) additional probability density plots and plot of state splitting sequence for Section 4.3, (v) Viterbi path visualizations for the entire observation period and years 2005, 2006 and 2007 for Section 4.4, (vi) sojourn checks for subsystems in Section 4.5.Disclosure StatementThe authors report that there are no competing interests to declare.
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