Computer Science
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Max-Planck-Institut für Chemie, Postfach 3060, D-55020 Mainz, Germany; University of Bristol, Department of Earth Sciences, Wills Memorial Building, Queens Road, Bristol, BS8 1RJ, United Kingdom
Bristol Isotope Group, School of Earth Sciences, Wills Memorial Building, Queens Road, University of Bristol, Bristol BS8 1RJ, UK
Max-Planck-Institut für Chemie, Postfach 3060, D-55020 Mainz, Germany
University of Bristol, Department of Earth Sciences, Wills Memorial Building, Bristol, BS8 1RJ, United Kingdom; Max-Planck-Institut für Chemie, Postfach 3060, D-55020 Mainz, Germany
Continental geochemical signatures in dacites from Iceland and implications for models of early Archaean crust formation
Reply to comment by E. Martin, M. Martin, and O. Sigmarsson on “Continental geochemical signatures in dacites from Iceland and implications for models of early Archaean crust formation” by M. Willbold, E. Hegner, A. Stracke, and A. Rocholl
Slab components in the Mariana arc: Light, heavy and novel
The tungsten isotopic composition of the Earth's mantle before the terminal bombardment
Upper and lower continental crust in the sources of ocean island basalts—isotopic and chemical constraints
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