The 2009-2010 eruption of Gaua (Vanuatu archipelago): eruptive dynamic and unsuspected strong halogens source
Bani Philipson, Boudon Georges, Balcone-Boissard Hélène, Delmelle Pierre, Quiniou Thomas, Lefevre Jérôme, Garaebiti Bule Esline, Shinohara Hiroshi, Lardy Michel. 2016. .
ARTICLE, (2016 ) - PUBLISHEDVERSION - English (en-GB)
OPENACCESS -
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Audience : OTHER
HAL CCSD, Elsevier
Sujet
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Domaines
Géologie, Volcanologie, Sciences de la Terre
Description
International audience Gaua, a little known volcano in the northern part of Vanuatu archipelago, went through a long term eruptive activity between September 2009 and July 2010. The eruption started by a phreatic to phreatomagmatic activity which progressively shifted into a magmatic discharge. The first eruptive phase involved the hydrothermal system in place. The latter was likely influenced by seawater seepage, leading to the formation of anhydrite. Magma involved hereafter this opening phase is of basaltic andesite and basaltic trachyandesite composition (high K calc-alkaline series), typical of the northern part of the Vanuatu archipelago. The 2009–2010 activity discharged at least 184 kt of SO2 and a significant amount of halogens (72 kt Cl and 217 kt F). Such halogen releases indicate that Gaua is a strong source of halogens into the atmosphere. High and sustained amount of F discharges are known to induce health issues and should not be ignored on Gaua island.During this eruption the quiescent and voluminous Lake Letas was slightly affected by the eruption. Nevertheless the hydrothermal discharge point into the lake, situated on the southeastern part of Mt. Garet appeared to be relatively active. At this particular location rock forming elements, leached out from volcanic rock by acid fluids released by the new intrusion of magma, were discharged along with anions into Lake Letas. This release has triggered localized chemistry changes in the lake. We speculate that this discharge has also disturbed the bottom water in a limited perimeter, remobilizing reduced Fe to the surface and subsequently triggering the change in the water color by Fe oxidation.
Auteurs
Bani, Philipson, Boudon, Georges, Balcone-Boissard, Hélène, Delmelle, Pierre, Quiniou, Thomas, Lefevre, Jérôme, Garaebiti Bule, Esline, Shinohara, Hiroshi, Lardy, Michel
Contributeurs
Laboratoire Magmas et Volcans (LMV) ; Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Institut de Recherche pour le Développement et la société-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Observatoire de Physique du Globe de Clermont-Ferrand (OPGC) ; Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Clermont Auvergne [2017-2020] (UCA [2017-2020])-Centre National de la Recherche Scientifique (CNRS), Center for Volcanology and Geological Hazard Mitigation, Institut de Physique du Globe de Paris (IPGP) ; Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Institut des Sciences de la Terre de Paris (iSTeP) ; Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Earth and Life Institute [Louvain-La-Neuve] (ELI) ; Université Catholique de Louvain = Catholic University of Louvain (UCL), Pôle Pluridisciplinaire de la Matière et de l'Environnement (PPME) ; Université de la Nouvelle-Calédonie (UNC), Laboratoire d'Etudes en Géophysique et Océanographie Spatiales (LEGOS NOUMEA) ; Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement [IRD] : UR065-Centre National de la Recherche Scientifique (CNRS), Vanuatu Geohazards Observatory Port Vila, Institute of Geology and Geoinformation (Geological Survey of Japan) ; National Institute of Advanced Industrial Science and Technology (AIST), Institut de Recherche pour le Développement (IRD [Nouvelle-Calédonie])
Sources
ISSN: 0377-0273, Journal of Volcanology and Geothermal Research, https://hal.science/hal-01402841, Journal of Volcanology and Geothermal Research, 2016, 322, pp.63-75. ⟨10.1016/j.jvolgeores.2015.06.023⟩
Relation
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jvolgeores.2015.06.023
Couverture
Vanuatu, Port Vila
