三维球形 ETAS 模型:阿拉斯加-阿留申地区案例研究

Yongbo Li, J. Zhuang, Shi Chen, Yicun Guo, Z. Xiong
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摘要

本研究提出了球形流行型余震序列(ETAS)模型的次中心版本,将次中心深度信息纳入球形 ETAS 模型,并将其应用于阿拉斯加-阿留申地区的地震数据。我们利用随机重建技术对模型进行了验证,并说明了选择空间概率密度函数的理由。随后,我们估算了研究区域的背景地震和后代地震的三维空间变化,发现大多数地震群位于浅层区域。此外,我们还发现了人工效应引起的背景地震的明显时间变化。与三维余震序列模型(3D-ETAS)和球形余震序列模型(SETAS)相比,新的三维余震序列模型能更好地描述全球高纬度地区的三维地震。
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A 3D Spherical ETAS Model: A Case Study in the Alaska-Aleutian Region
This study proposes a hypocentral version of the spherical epidemic-type aftershock sequence (ETAS) model by incorporating hypocentral depth information into the spherical ETAS model and applies it to earthquake data from the Alaska-Aleutian area. We validate the model using the stochastic reconstruction techniques and illustrate the rationale behind selecting the spatial probability density function. Subsequently, we estimate the 3D spatial variations of the background and offspring seismicity in the study region, revealing that the majority of clusters are located in shallow regions. We also identify an apparent temporal change in the background seismicity caused by artificial effects. Compared with the 3D-ETAS and spherical version of the epidemic-type aftershock sequence (SETAS) models, the new 3D-SETAS model provides a better description of 3D seismicity in high-latitude regions globally.
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