Authors
Víctor Villasante-Marcos, Anthony Finizola, Rafael Abella, Stéphanie Barde-Cabusson, María José Blanco, Beatriz Brenes, Víctor Cabrera, Benito Casas, Pablo De Agustín, Fabio Di Gangi, Itahiza Domínguez, Olaya García, Almudena Gomis, Juan Guzmán, Ilazkiñe Iribarren, Guillaume Levieux, Carmen López, Natividad Luengo-Oroz, Isidoro Martín, Manuel Moreno, Stavros Meletlidis, Julie Morin, David Moure, Jorge Pereda, Tullio Ricci, Enrique Romero, Claudia Schütze, Barbara Suski-Ricci, Pedro Torres, Patricia Trigo
Publication date
2014/2/15
Journal
Journal of Volcanology and Geothermal Research
Volume
272
Pages
59-77
Publisher
Elsevier
Description
An extensive self-potential survey was carried out in the central volcanic complex of Tenerife Island (Canary Islands, Spain). A total amount of ~ 237 km of profiles with 20 m spacing between measurements was completed, including radial profiles extending from the summits of Teide and Pico Viejo, and circular profiles inside and around Las Cañadas caldera and the northern slopes of Teide and Pico Viejo. One of the main results of this mapping is the detection of well-developed hydrothermal systems within the edifices of Teide and Pico Viejo, and also associated with the flank satellite M. Blanca and M. Rajada volcanoes. A strong structural control of the surface manifestation of these hydrothermal systems is deduced from the data, pointing to the subdivision of Teide and Pico Viejo hydrothermal systems in three zones: summit crater, upper and lower hydrothermal systems. Self-potential maxima related to …
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