RT info:eu-repo/semantics/bookPart
T1 From Magma Source to Volcanic SinkUnder Tagoro Volcano (El Hierro,Canary Islands): Petrologic,Geochemical and PhysiographicEvolution of the 2011–2012 Submarine Eruption
A1 Martín Luis, María Candelaria
A1 Álvarez-Valero, Antonio M.
A1 Sánchez Guillamón, Olga
A1 Navarro, Irene
A1 Albert, Helena
A1 Polo Sánchez, Antonio
A1 Lozano Rodríguez, José A.
A1 Geyer, Adelina
A1 Martí, Joan
A1 Ban, Masao
A1 Gómez Ballesteros, María
A1 Catalán, Manuel
A1 García, Natalia
A1 Fraile-Nuez, Eugenio
A1 Casillas, Ramón
A1 Martín Luis, María C.
A1 Palomino, Desirée
A1 Vázquez, Juan T.
A1 López González, Nieves
A1 Hernández Barreña, Daniel
A1 Núñez Guerrero, Elena
K1 Canary Islands
K1 Holocene Rift Volcanism
K1 Tagoro Submarine Volcano
K1 Ocean Island Magmatism
K1 Submarine Eruption
K1 Geology
K1 Geophysics
K1 Geodesy, Natural Hazards,
K1 Geochemistry
AB Active volcanoes are key laboratories to carryout detailed research -and monitoring- aboutthe history of magmas before, during and aftereruptions. Tagoro, the submarine active volcano at El Hierro Island (Canary archipelago),is a highly favorable case to assess andmonitor its daily ongoing behaviour, as wellas to study the links between the processes ofmagma genesis occurring at depth and theirderived eruptive events at the surface. In thisinterdisciplinary research we combine newresults of classical petrology (petrography,geochemistry, and thermodynamics) on thevolcanic products expelled by Tagoro duringthe 2011–2012 eruption, with a highresolution (5 m grid) bathymetry model carried out during 2017, and recent data frommagnetometry, to refine the current knowledge of this eruption. Our results mainlyreveal (i) slight magma differentiation andmixing processes at c. 12 km depth during acontinuous eruptive pulse; (ii) a similar magmatic evolution and residence times at depthbetween previous and 2011–2012 eruptionson the island; (iii) an insignificant interactionof external fluids with the magma at depth orwithin the ascent conduit; (iv) a present-daymagnetometric anomaly under the Tagoro’sarea; (v) a minimum volume estimate for themagma withdrawn from the plumbing systemat depth.
PB Springer
SN 978-3-031-35134-1
SN Series ISSN 2195-3589
YR 2023
FD 2023
LK http://riull.ull.es/xmlui/handle/915/35721
UL http://riull.ull.es/xmlui/handle/915/35721
LA Inglés
DS Repositorio institucional de la Universidad de La Laguna
RD 22-nov-2024