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Max-Planck-Institut für Chemie, Postfach 3060, D-55020 Mainz, Germany; Geological Sciences Department, The University of Texas at Austin, 1, University Station C1100, Austin, TX, 78712-0254, USA
Department of Geological Sciences, University of Texas at Austin, 1 University Station C1100, Austin, TX 78712, USA
Department of Geological Sciences, Jackson School of Geosciences, University of Texas, Austin, TX 78712, USA
Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX 78751, USA
University of Texas, Department of Geological Sciences, Austin, TX 78712, USA of Geological Science, Jackson School of Geoscience, University of Texas, Austin, TX, USA
Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC, USA
Max-Planck-Institut für Chemie, Postfach 3060, 55020, Mainz, Germany
Max-Planck-Institut für Chemie, Postfach 3060, 55020 Mainz, Germany
Ancient recycled mantle lithosphere in the Hawaiian plume: Osmium Hafnium isotopic evidence from peridotite mantle xenoliths
Chlorine-potassium variations in melt inclusions from Raivavae and Rapa, Austral Islands: constraints on chlorine recycling in the mantle and evidence for brine-induced melting of oceanic crust
Constraints on Melt/Lithosphere and Melt/Hydrosphere Interaction from the Volatile Budgets of Melt Inclusions from the Austral Islands
Constraints on the age of the Earth’s inner core and the origin of the 186Os/188Os “core signal” in plume-derived lavas
Constraints on the coupled thermal evolution of the Earth's core and mantle, the age of the inner core, and the origin of the 186Os/188Os “core signal” in plume-derived lavas
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