Physics
Scientist
Geosciences Montpellier, CNRS & Université Montpellier 2, CC.060, Pl. Eugène Bataillon, Montpellier, F-34095, France
Géosciences Montpellier, Université Montpellier II, CNRS, Montpellier, France
Géosciences Montpellier, CNRS, Université Montpellier II, F-34095 Montpellier Cedex 5, France
Laboratoire de Tectonophysique, Université Montpellier 2, Montpellier, France
Laboratoire de Tectonophysique, CNRS and Université Montpellier II, France
Laboratoire de Tectonophysique, CNRS and Université Montpellier II, 34095 Montpellier cedex 5, France. Now at Earth Sciences, South Illinois University, Carbondale, IL 62901, USA
Géosciences Montpellier, CNRS & Université Montpellier 2, 34095 Montpellier, France
Laboratoire de Tectonophysique, ISTEEM, CNRS, Université Montpellier 2, France
Laboratoire de Tectonophysique, Université Montpellier II-CNRS, Place Eugène Bataillon, F-34095, Montpellier Cedex 5, France
Géosciences Montpellier, CNRS & Université Montpellier 2, F-34095 Montpellier cedex5, France
School of Earth Sciences, University of Leeds, LS2 9JT, Leeds, UK
Laboratoire Tectonophysique, ISTEEM, CNRS / Université de Montpellier II, 34095, Montpellier, France
Université Montpellier 2 & CNRS, UMR 5243, Géosciences Montpellier, Montpellier, France
Géosciences Montpellier, Université Montpellier II, CNRS, Place Eugène Bataillon 34095 Montpellier cedex 5, France
Université Montpellier II, Géosciences Montpellier, CNRS, UMR 5243, Place Eugène Bataillon, CC060 34095 Montpellier, France
Laboratoire de Tectonophysique, CNRS / Université de Montpellier II, F34095 Cedex 5, Montpellier, France
Comment on the article “Probability of radial anisotropy in the deep mantle” by Visser et al. (2008) EPSL 270:241 250
Continental rifting parallel to ancient collisional belts: an effect of the mechanical anisotropy of the lithospheric mantle
Deformation and melt transport in a highly depleted peridotite massif from the Canadian Cordillera: Implications to seismic anisotropy above subduction zones
Deformation and seismic anisotropy of the lithospheric mantle in the southeastern Carpathians inferred from the study of mantle xenoliths
Deformation, static recrystallization, and reactive melt transport in shallow subcontinental mantle xenoliths (Tok Cenozoic volcanic field, SE Siberia)
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