Events
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- 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
- LLSVP can be explained by recycled oceanic crust
- Deep magma ocean changes Earth's atmosphere
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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
Tel: +49-(0) 921 55 3700 / 3766, Fax: +49-(0) 921 55 3769, E-mail: bayerisches.geoinstitut(at)uni-bayreuth.de