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Willkommen am Bayerischen Geoinstitut Forschungsinstitut für Experimentelle Geochemie und Geophysik (BGI) Universität Bayreuth |
Staff scientist position
Stagnation of subducting slabs in the transition zone due to slow diffusion in majoritic garnet.
Water and hydrogen are immiscible in Earth's mantle.
Effect of iron oxidation state on the electrical conductivity of the Earth’s lower mantle.
The oxidation state of the mantle and the extraction of carbon from Earth’s interior.
Perovskite-like Mn2O3: a path to new manganites.
Origin of the terrestrial noble-gas signature.
Generation of 6 Mbars using DAC.
Thermal conductivity of liquid Fe alloys - thermal state of Earth's core.