Resumen
Cotopaxi Volcano showed an increased activity since April 2015 and evolved into its eventual mild eruption in August 2015. In this work we use records from a broadband seismic station located at less than 4 km from the vent that encompass data from April to December of 2015, to detect and study low-frequency seismic events. We applied unsupervised learning schemes to group and identify possible premonitory low-frequency seismic families. To find these families we applied a two-stage process in which the events were first separated by their frequency content by applying the k-means algorithm to the spectral density vector of the signals and then were further separated by their waveform by applying Correntropy and Dynamic Time Warping. As a result, we found a particular family related to the volcano's state of activity by exploring its time distribution and estimating its events' locations.
Idioma original | Inglés |
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Número de artículo | 6526898 |
Publicación | International Journal of Geophysics |
Volumen | 2019 |
DOI | |
Estado | Publicada - 22 may. 2019 |
Nota bibliográfica
Publisher Copyright:© 2019 Juan C. Anzieta et al.