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
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