- 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
- 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
- First Observation of Hydrogen-Hydrogen Interactions in Metal Hydrides at Multi-Megabar Pressures
- Magnetism in subduction zones
- Spin-induced multiferroicity in the binary perovskite manganite Mn2O3
- Pressure tuning of charge ordering in iron oxide
- Breaking the secrets of icy protons
- Oxidised garnets from the Earth's transition zone
- Nuclear Magnetic Resonance breaks through the barriers of high pressure
- Stability of iron-bearing carbonates in the deep Earth's interior
- Compressional pathways of α-cristobalite, structure of cristobalite X-I, and towards the understanding of seifertite formation
- Continental crust formation on early Earth controlled by intrusive magmatism
- Evidence for a Fe3+-rich pyrolitic lower mantle from (Al,Fe)-bearing bridgmanite elasticity data
- Highly siderophile elements were stripped from Earth’s mantle by iron sulfide segregation
- Redox-induced lower mantle density contrast and effect on mantle structure and primitive oxygen
- Stability of Fe, Al-bearing bridgmanite in the lower mantle and synthesis of pure Fe-bridgmanite
- Terapascal static pressure generation with ultrahigh yield strength nanodiamond.
- Charge ordering transition in iron oxide Fe4O5 involving competing dimer and trimer formation.
- Fate of MgSiO3 melts at core–mantle boundary conditions.
- The most incompressible metal osmium at static pressures above 750 gigapascals.
- Accretion and differentiation of the terrestrial planets with implications for the compositions of early-formed Solar System bodies and accretion of water.
- High Poisson’s ratio of Earth’s inner core explained by carbon alloying.
- Slab stagnation in the shallow lower mantle linked to an increase in mantle viscosity.
- Lower-mantle water reservoir implied by the extreme stability of a hydrous aluminosilicate.
- Shock compression of stishovite and melting of silica at planetary interior conditions.
- Did life exist on Mars? New evidence from NanoSIMS analysis of organic carbon from the Tissint Martian meteorite.
- Mixing at mid-ocean ridges controlled by small-scale convection and plate motion.
- Highly siderophile elements in Earth’s mantle as a clock for the Moon-forming impact.
- Discovery of a Superhard Iron Tetraboride Superconductor.
- Strong inheritance of texture between perovskite and post-perovskite in the D" layer.
- Small effect of water on upper mantle rheology based on silicon self-diffusion coefficients.
- 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.
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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