2018
DOI: 10.1038/s41561-018-0272-8
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Similarity of fast and slow earthquakes illuminated by machine learning

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Cited by 144 publications
(161 citation statements)
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References 28 publications
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“…We find that the best features identified in Cascadia follow very similar patterns compared to those identified in the laboratory. In the case of laboratory slow slip events, the most important feature by far for forecasting failure time is the seismic power 13,34 , shown in Fig. 3c.…”
Section: Seismic Power Analysis and The Occurrence Of Slow Slip Inmentioning
confidence: 99%
“…We find that the best features identified in Cascadia follow very similar patterns compared to those identified in the laboratory. In the case of laboratory slow slip events, the most important feature by far for forecasting failure time is the seismic power 13,34 , shown in Fig. 3c.…”
Section: Seismic Power Analysis and The Occurrence Of Slow Slip Inmentioning
confidence: 99%
“…Our XGBoost model isolates consistent frequencies present throughout the majority of the eruptions in our data set, with a surprisingly good performance for a single station. This type of analysis could potentially be utilized to search for previously undetected precursory pre-eruptive signals, in a similar approach to Rouet-Leduc, Hulbert, and Johnson (2018), and provide a path toward estimating the onset of eruptions, although it is important to note that there is little evidence for a continuously emitting source at the Piton de la Fournaise, unlike at the Juan de Fuca plate.…”
Section: Discussionmentioning
confidence: 99%
“…The aim here is to capture distributions of the seismic data within the time windows and relationships across different frequency bands for a given window. This has been shown to be an effective technique to parametrize geophysical time series data in various settings such as simulations (Ren et al, ), laboratory experiments (Hulbert et al, ; Rouet‐Leduc et al, ; Rouet‐Leduc, Hulbert, Bolton, et al, ), and real Earth (Rouet‐Leduc, Hulbert, & Johnson, ). In this case, these features consist of a range of percentiles and the range of the data, as well as normalized and nonnormalized higher‐order moments (see the supporting information for table describing features).…”
Section: Regional Settingmentioning
confidence: 99%
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“…As shown in [26] instantaneous statistical characteristics of AD appear as a "fingerprint" of the fault zone stress state. The variance of the seismic signal is the most important feature, although other statistical characteristics are also important [26,29,31]. The authors of [13] stressed that the kurtosis of the acoustic signal is an additional powerful feature for the prediction of TTF.…”
Section: Feature Engineeringmentioning
confidence: 99%