细心深度学习模型揭示兴都库什-帕米尔高原地区地壳和中间地震活动性增强

Satyam Pratap Singh , Vipul Silwal
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引用次数: 0

摘要

兴都库什-帕米尔地区(HKPR)具有复杂的持续变形、独特的板块几何形状和中等地震活动的特点。近几十年来,大量地震学数据的可用性促使人们使用深度学习算法来提取有价值的见解。在这项研究中,我们提出了一种全自动的方法来扩充香港公共关系中的地震目录。我们的方法利用基于注意力机制的深度学习架构来同时检测事件、执行相位拾取和估计幅度。我们将该模型应用于该地区83个站点的10个月数据集(2013年1月至2013年10月)。利用一个稳健的标准来评估模型的概率,我们将不同台站的相位关联起来,并精确定位该地区的地震位置。我们的研究结果显示了显著的增强,揭示了比国际地震中心(ISC)目录中先前记录的地震多出近4.5倍的地震。这些新探测到的事件中有一个值得注意的部分属于极低震级地震(<;3)的类别,而ISC目录中没有这类地震。值得注意的是,我们的时空分析揭示了帕米尔西部新构造北向和东北向断层以及瓦赫什冲断系统和达尔瓦兹-卡拉库尔断层沿线地壳地震活动的集中。这些发现强调了未来地震灾害的潜在来源。此外,我们扩大的地震目录有助于更深入地了解HKPR中地壳和中间地震活动之间的相互作用,从而揭示欧亚-印度板块相互作用引起的变形和活动断层作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Enhanced crustal and intermediate seismicity in the Hindu Kush-Pamir region revealed by attentive deep learning model

The Hindu Kush-Pamir region (HKPR) is characterized by complex ongoing deformation, unique slab geometry, and intermediate seismic activity. The availability of extensive seismological data in recent decades has prompted the use of deep learning algorithms to extract valuable insights. In this study, we present a fully automated approach for augmenting earthquake catalogue within the HKPR. Our method leverages an attention mechanism-based deep learning architecture to simultaneously detect events, perform phase picking, and estimate magnitudes. We applied this model to a ten-month dataset (January 2013–October 2013) from 83 stations in the region. Utilizing a robust criterion to evaluate the model's probabilities, we associated phases at different stations and pinpointed earthquake locations in the region. Our results demonstrate a significant enhancement, revealing nearly four and a half times more earthquakes than previously documented in the International Seismological Center (ISC) catalogue. A notable portion of these newly detected events falls within the category of very low-magnitude earthquakes (<3), which were absent in the ISC catalogue. Notably, our spatiotemporal analysis reveals a concentration of crustal seismicity along poorly mapped neotectonic north and northeast-oriented faults in the western Pamir, as well as the Vakhsh Thrust System and the Darvaz Karakul Fault. These findings underscore potential sources of future seismic hazards. Furthermore, our expanded earthquake catalogue facilitates a deeper understanding of the interplay between crustal and intermediate seismic activity in the HKPR, shedding light on the deformation and active faulting resulting from Eurasian-Indian plate interactions.

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