Bayerisches Geoinstitut

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Welcome to the
Bavarian Research Institute of
Experimental Geochemistry and Geophysics (BGI)
University of Bayreuth

Events

Research Highlights

New constraints on Ti diffusion in quartz and the priming of silicic volcanic eruptions
Mid-mantle dynamics explained by the curved post-garnet transition
The mid-mantle viscosity jump explained by bridgmanite grain size variation
Water cycling into the lower mantle by hydrous aluminous silica phases
New materials synthesized at terapascal pressures for the first time
Depressed 660-km discontinuity caused by akimotoite-bridgmanite transition

DFG Core Facility for High Pressure Research

The Emmy Noether Research Group QuakeID aims at deciphering the rupture processes of deep earthquakes which occur at depths larger than 60 km.

Chemistry and transport properties of bridgmanite controlling lower-mantle dynamics. A research project funded by the European Research Council (ERC).

Master of Science in Experimental Geosciences.
For students who want to do research right from the beginning.

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Bayerisches Geoinstitut, University of Bayreuth, 95440 Bayreuth, Germany
Tel: +49-(0) 921 55 3700 / 3766, Fax: +49-(0) 921 55 3769, E-mail: bayerisches.geoinstitut(at)uni-bayreuth.de