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<datestamp>2018-01-11</datestamp>
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<title lang=en>South Pacific hotspot swells dynamically supported by mantle flows</title>
<creator>Adam, Claudia</creator>
<creator>Yoshida, Masaki</creator>
<creator>Isse, Takehi</creator>
<creator>Suetsugu, Daisuke</creator>
<creator>Fukao, Yoshio</creator>
<creator>Barruol, Guilhem</creator>
<contributor>Centro de Geofísica de Évora ; Universidade de Évora</contributor>
<contributor>Institute for Research on Earth Evolution (IFREE) (IFREE) ; Japan Agency for Marine-Earth Science and Technology (JAMSTEC)</contributor>
<contributor>Earthquake Research Institute, The University of Tokyo, 1-1-1, Yayoi, Bunkyo, 113-0032 Tokyo, Japan</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire GéoSciences Réunion (LGSR) ; Université de la Réunion (UR) - Institut de Physique du Globe de Paris</contributor>
<description>International audience</description>
<source>ISSN: 0094-8276</source>
<source>EISSN: 1944-8007</source>
<source>Geophysical Research Letters</source>
<publisher>American Geophysical Union</publisher>
<identifier>hal-01236157</identifier>
<identifier>http://hal.univ-reunion.fr/hal-01236157</identifier>
<identifier>http://hal.univ-reunion.fr/hal-01236157/document</identifier>
<identifier>http://hal.univ-reunion.fr/hal-01236157/file/Adam_South_Pacific_Superswell_GRL2010.pdf</identifier>
<source>http://hal.univ-reunion.fr/hal-01236157</source>
<source>Geophysical Research Letters, American Geophysical Union, 2010, 〈10.1029/2010GL042534〉</source>
<identifier>DOI : 10.1029/2010GL042534</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2010GL042534</relation>
<language>en</language>
<subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The dynamics of mantle plumes and the origin of their associated swells remain some of the most controversial topics in geodynamics. Here we construct a numerical model of the mantle flow beneath the French Polynesia region. Our study is based on a new regional seismic tomography model, which high resolution allows obtaining information at the scale of plumes. We find excellent correlations between the observed and the modeled dynamic swells, between the modeled flow pattern and the active volcanism and between the buoyancy fluxes obtained from our numerical model and the ones deduced from the swells morphology. These outstanding fits reveal for the first time that a direct link exists between the surface observations and mantle flows.</description>
<date>2010</date>
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