Physics
Scientist
Max-Planck-Institut für Chemie, Abteilung Geochemie, Mainz, für Chemie, Abt. Geochemie, Postfach 3060, 55020, Mainz, Germany
Max-Planck-Institut für Chemie, Abteilung Geochemie, Postfach 3060, D-55020 Mainz, Germany; Woods Hole Oceanographic Institution, Geology and Geophysics, Woods Hole, MA 02543, USA
Woods Hole Oceanographic Institution, Geology & Geophysics, Woods Hole, MA 02543, USA; Centre de Recherches Pétrographiques et Géochimiques, CNRS-Nancy Université, BP 20, F-54501 Vandoeuvre-lès-Nancy, France;
B isotope composition of Gorgona komatiites: Do melt inclusions support a subduction-related origin?
Boron isotopic composition of olivine-hosted melt inclusions from Gorgona komatiites, Colombia: New evidence supporting wet komatiite origin
Discovery of whitlockite in mantle xenoliths: Inferences for water- and halogen-poor fluids and trace element residence in the terrestrial upper mantle
Enriched and depleted primitive melts included in olivine from Icelandic tholeiites: origin by continuous melting of a single mantle column
Enriched, HIMU-type peridotite and depleted recycled pyroxenite in the Canary plume: A mixed-up mantle
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