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Large-scale inflation of Tungurahua volcano (Ecuador) revealed by Persistent Scatterers SAR interferometry

Authors :
Hervé Jomard
Johann Champenois
Hugo Yepes
Laurence Audin
Alexandra Alvarado
Virginie Pinel
Stéphane Baize
Andrew Hooper
Institut de Radioprotection et de Sûreté Nucléaire (IRSN)
Institut des Sciences de la Terre (ISTerre)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement [IRD] : UR219-PRES Université de Grenoble-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)
University of Leeds
instituto Geofísico
Escuela Politécnica Nacional (EPN)
European Space Agency, ESA
Source :
Geophysical Research Letters, Geophysical Research Letters, 2014, 41 (16), pp.5821-5828. ⟨10.1002/2014GL060956⟩, Geophysical Research Letters, American Geophysical Union, 2014, 41 (16), pp.5821-5828. ⟨10.1002/2014GL060956⟩
Publication Year :
2014
Publisher :
HAL CCSD, 2014.

Abstract

International audience; The Tungurahua volcano, in Ecuador, has been experiencing a substantial activity period since 1999, with several eruptions, including those of 2006 and 2008. We use a persistent scatterers approach to analyze a time series of Envisat synthetic aperture radar (SAR) data over the period 2003-2009, to investigate surface deformation in the region of the volcano. We measure a continuous large-scale uplift with a maximum line of sight displacement rate of about 8 mm/yr, which is the first evidence of a sustained inflation in the Andes for an active volcano encompassing several eruptions. We model this signal as magma emplacement in a permanent storage zone at 11.5 km below sea level, with a net inflow rate of 7 million m3/yr. The paroxysmal eruptions in 2006 and 2008 did not seem to disrupt this long-term signal. However, we observe significant deformation during the 2006 eruption consistent with an additional intrusion of 4.5 million m3 of magma. © 2014. American Geophysical Union.

Details

Language :
English
ISSN :
00948276 and 19448007
Database :
OpenAIRE
Journal :
Geophysical Research Letters, Geophysical Research Letters, 2014, 41 (16), pp.5821-5828. ⟨10.1002/2014GL060956⟩, Geophysical Research Letters, American Geophysical Union, 2014, 41 (16), pp.5821-5828. ⟨10.1002/2014GL060956⟩
Accession number :
edsair.doi.dedup.....dec6d596efe47465b40ec000cec35800
Full Text :
https://doi.org/10.1002/2014GL060956⟩