- 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
- Synthesis of paracrystalline diamond
- Dry metastable olivine and slab deformation in a wet subducting slab
- Novel experiments at BGI explain the sharpness of the 660 km discontinuity
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Bayerisches Geoinstitut, Universität Bayreuth, 95440 Bayreuth, Deutschland
Tel: +49-(0) 921 55 3700 / 3766, Fax: +49-(0) 921 55 3769, E-mail: bayerisches.geoinstitut(at)uni-bayreuth.de
Tel: +49-(0) 921 55 3700 / 3766, Fax: +49-(0) 921 55 3769, E-mail: bayerisches.geoinstitut(at)uni-bayreuth.de