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Dynamic strain determination using fibre-optic cables allows imaging of seismological and structural features

机译:使用光纤电缆动态应变确定可对地震和结构特征进行成像

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摘要

Natural hazard prediction and efficient crust exploration require dense seismic observations both in time and space. Seismological techniques provide ground-motion data, whose accuracy depends on sensor characteristics and spatial distribution. Here we demonstrate that dynamic strain determination is possible with conventional fibre-optic cables deployed for telecommunication. Extending recently distributed acoustic sensing (DAS) studies, we present high resolution spatially un-aliased broadband strain data. We recorded seismic signals from natural and man-made sources with 4-m spacing along a 15-km-long fibre-optic cable layout on Reykjanes Peninsula, SW-Iceland. We identify with unprecedented resolution structural features such as normal faults and volcanic dykes in the Reykjanes Oblique Rift, allowing us to infer new dynamic fault processes. Conventional seismometer recordings, acquired simultaneously, validate the spectral amplitude DAS response between 0.1 and 100 Hz bandwidth. We suggest that the networks of fibre-optic telecommunication lines worldwide could be used as seismometers opening a new window for Earth hazard assessment and exploration.
机译:自然灾害的预测和有效的地壳勘探需要在时间和空间上进行密集的地震观测。地震技术提供地面运动数据,其准确性取决于传感器的特性和空间分布。在这里,我们证明了使用用于电信的常规光纤电缆可以确定动态应变。扩展了最近的分布式声感测(DAS)研究,我们提出了高分辨率的空间无混叠宽带应变数据。我们在冰岛西南部的雷克雅内斯半岛沿15公里长的光纤电缆布置,以4米的间隔记录了来自自然和人造来源的地震信号。我们以前所未有的分辨率确定了雷克雅尼斯斜裂谷中的正常断层和火山堤等结构特征,从而可以推断出新的动态断层过程。同时采集的常规地震仪记录可验证0.1至100 Hz带宽之间的频谱幅度DAS响应。我们建议,可以将全世界的光纤通信线路网络用作地震仪,为评估地球灾害和探索打开新的窗口。

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