Physics
Scientist
Steinmann Institut, Endogene Prozesse, Universität Bonn, Poppelsdorfer Schloss, 53115 Bonn, Germany
Steinmann Institut, University of Bonn, Universität Bonn, Poppelsdorfer Schloss, 53115 Bonn, Germany; Now at: Boliden Mineral AB, 93681 Boliden, Sweden.;
Carbonate veins trace seawater circulation during exhumation and uplift of mantle rock: Results from ODP Leg 209
First evidence for high-temperature off-axis venting of deep crustal/mantle heat: The Nibelungen hydrothermal field, southern Mid-Atlantic Ridge
The Earth’s tungsten budget during mantle melting and crust formation
The elemental budget of W during mantle melting and crust formation
The influence of small-scale mantle heterogeneities on Mid-Ocean Ridge volcanism: Evidence from the southern Mid-Atlantic Ridge (7°30′S to 11°30′S) and Ascension Island
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