EGU25-18834, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-18834
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 10:45–12:30 (CEST), Display time Monday, 28 Apr, 08:30–12:30
 
Hall X4, X4.76
Revealing the hidden seismicity of Tenerife (Canary Islands) through machine learning and cross-correlation
Luca D'Auria1,2, Lucía Mesa Jiménez3, Ismael Santos Campos4, Aarón Álvarez Hernández1, Rubén García Hernández1, David Martínez van Dorth1,2, Víctor Ortega Ramos1, Germán D. Padilla Hernández1,2, and Nemesio M. Pérez Rodríguez1,2
Luca D'Auria et al.
  • 1Instituto Volcanológico de Canarias (INVOLCAN), 38400 Puerto de la Cruz, Tenerife, Canary Islands, Spain
  • 2Instituto Tecnológico y de Energías Renovables (ITER), 38600 Granadilla de Abona, Tenerife, Canary Islands, Spain.
  • 3Universidad de Granada, 18071, Granada, España
  • 4Universidad de La Laguna, 38200 San Cristóbal de La Laguna, Tenerife, Spain

In recent years, the development of techniques based on integrated machine learning techniques with traditional methods like cross-correlation has dramatically improved the capability of detection, location and characterisation of seismic events.

Machine learning-based techniques have been applied to improve earthquake catalogues, aiding seismicity analysis in different geodynamic contexts. These techniques are especially valuable in volcanic and geothermal contexts, where volcano-tectonic earthquakes and long-period events have low magnitude, often preventing a successful manual analysis. Since 2016, the island of Tenerife has been affected by increased seismicity and gas emissions from the crater of Teide volcano, the most prominent feature of the island of Tenerife. We applied the software Qseek (https://github.com/pyrocko/qseek) to enhance the seismic catalogue based on manual detections in Tenerife.

This reanalysis of Tenerife's seismic dataset revealed intense seismicity related to episodes of magmatic fluid injection into the upper crust. Subsequently, high-resolution relocation techniques based on the software GrowClust (https://github.com/dttrugman/GrowClust) imaged the spatial pattern of the hypocenters, highlighting sources of magmatic fluid injection into the hydrothermal system of Tenerife and the subsequent response of the upper crust to this disturbance.

How to cite: D'Auria, L., Mesa Jiménez, L., Santos Campos, I., Álvarez Hernández, A., García Hernández, R., Martínez van Dorth, D., Ortega Ramos, V., Padilla Hernández, G. D., and Pérez Rodríguez, N. M.: Revealing the hidden seismicity of Tenerife (Canary Islands) through machine learning and cross-correlation, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-18834, https://doi.org/10.5194/egusphere-egu25-18834, 2025.