Ambient Noise Tomography studies for geothermal exploration in the Canary Islands

Iván Cabrera-Pérez; Luca D’Auria; Jean Soubestre; David Martínez van Dorth; Germán Cervigón-Tomico; Alba Martín-Lorenzo; Monika Przeor; Rubén García-Hernández; Víctor Ortega; Germán D. Padilla; José Barrancos; Eleazar  Padrón; Nemesio M. Pérez

doi:10.21701/bolgeomin/134.3/001

Autores/as

Iván Cabrera-Pérez Instituto Volcanológico de Canarias (INVOLCAN)
Luca D’Auria Instituto Volcanológico de Canarias (INVOLCAN)
Jean Soubestre Université Grenoble Alpes
David Martínez van Dorth Instituto Tecnológico y de Energías Renovables (ITER)
Germán Cervigón-Tomico Instituto Volcanológico de Canarias (INVOLCAN)
Alba Martín-Lorenzo Instituto Volcanológico de Canarias (INVOLCAN)
Monika Przeor Instituto Tecnológico y de Energías Renovables (ITER)
Rubén García-Hernández Instituto Volcanológico de Canarias (INVOLCAN)
Víctor Ortega Instituto Volcanológico de Canarias (INVOLCAN)
Germán D. Padilla Instituto Volcanológico de Canarias (INVOLCAN)
José Barrancos Instituto Volcanológico de Canarias (INVOLCAN)
Eleazar Padrón Instituto Volcanológico de Canarias (INVOLCAN)
Nemesio M. Pérez Instituto Volcanológico de Canarias (INVOLCAN)

DOI:

https://doi.org/10.21701/bolgeomin/134.3/001

Palabras clave:

Tomografía de ruido sísmico, Exploración geotérmica, Gran Canaria, Tenerife, La Palma

Resumen

La tomografía de ruido sísmico es una técnica de exploración geofísica que ha mostrado ser muy eficiente para estudios a diferentes escalas y para múltiples propósitos, como la exploración geotérmica. En este artículo hacemos una introducción de esta técnica repasando sus diferentes pasos. También, se muestran algunos ejemplos de aplicaciones de estudios realizados en las Islas Canarias (concretamente en Tenerife, Gran Canaria y La Palma) con fines de exploración geotérmica. El estudio realizado en Gran Canaria muestra una serie de zonas de baja velocidad en la parte sur y este de la isla que podrían estar vinculadas a células convectivas. En Tenerife se ha observado una zona de baja velocidad que podría estar relacionada con un clay cap superficial que podría permitir el ascenso de gases a la superficie. Por último, el estudio realizado en La Palma muestra la existencia de dos zonas de baja velocidad en la parte sur de la isla que podrían estar vinculadas con zonas de arcillas hidrotermalizadas, lo que podría indicar una circulación de fluidos hidrotermales.

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Citas

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