Physics
Scientist
Department of Earth Sciences, The University of Western Ontario, London, Ontario, Canada. * Now at: Laboratoire de Dynamique des Systèmes Géologiques, Institut de Physique du Globe de Paris, Paris, France des sciences de la Terre et de l'Atmosphère, Centre de recherche en géochimie et en géodynamique, Université du Québec à Montréal, Montréal, Québec, Canada
GEOTOP-UQAM-McGill, University of Quebec, Montreal, Que., Canada H3C3P8
Department of Earth Sciences, University of Western Ontario, B&G Building, London, ON, Canada
GEOTOP, Université du Québec à Montréal, Montreal, Canada. University, Cambridge, MA
GEOTOP, Département des Sciences de la Terre et de l'Atmosphère, Université du Québec à Montréal CP 8888, succursale Centre-Ville, Montréal, Québec, Canada University, Cambridge, MA
Université de Paris, Paris, Frane
Department of Earth Sciences, University of Western Ontario, London, Ontario, Canada
Institut de Physique du Globe de Paris, Département de Sismologie, Paris, France
Department of Earth Sciences, The University of Western Ontario, London, Ontario, Canada. Department des Sciences de la Terre et de l'Atmosphere Universite du Quebec a Montreal, CP 8888, succursale Centre-Ville, Montreal, QC H3C 3P8 Canada Université du Québec à Montréal, Montreal, Quebec, Canada
The University of Western Ontario, Department of Earth Sciences, London, ON N6A 5B7 Canada
GEOTOP, Université du Québec à Montréal, Montréal, Québec, Canada H3C 3P8
Université du Québec à Montréal, GEOTOP, Département des Sciences de la Terre et de l'Atmosphère, CP 8888, succursale Centre-ville, Montréal, Québec, Canada H3C 3P8
Institut de Physique du Globe de Paris, Paris, France
GEOTOP, Département des Sciences de la Terre, Cp. 8888, succ. centre ville, Montréal, Québec, H3C-3P8, Canada. of Earth Sciences, University of Wester
A new inference of mantle viscosity based upon joint inversion of convection and glacial isostatic adjustment data
A reappraisal of postglacial decay times from Richmond Gulf and James Bay, Canada
A resonance in the Earth's obliquity and precession overthe past 20 Myr drivenbymantle convection
Constraining mantle flow with seismic and geodynamic data: A joint approach
Continent-Ocean Chemical Heterogeneity in the Mantle Based on Seismic Tomography
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