HelioWebDESY Deutsches Electronen-Synchrotron, Hamburg
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I[DESY Deutsches Electronen-Synchrotron, Hamburg]
PI["Parent Institutions (1)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (89)"]
CA["Linked Collaborating Authors (19)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
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Affiliated Works
sorted by decreasing year, and then by display-name
- Multielement geochemical investigations by SRXRF microprobe studies on tectite material: Evidence from the NE-Mexican Cretaceous/Tertiary record
- Geochemistry of K/T-boundary Chicxulub ejecta of NE-Mexico
- Reconstructing the Pore Space of Sand Samples
- Multi-Anvil Techniques in Conjunction With Synchrotron Radiation - MAX80 and MAX200x
- Effect of Water Activity on Mineral Reaction Overstepping at High P and T: Experimental Approach and Petrological Implications
- High-Pressure Falling Sphere Viscosimetry of Basaltic and Dacitic Rocks in Conjunction with Synchrotron Radiation
- Plastic deformation of polycrystalline MgO up to 1250 K and 65 GPa
- Zircon solubility and of Zr species in subduction zone fluids
- Bromine release during Plinian eruptions along the Central American Volcanic Arc
- A novel in situ approach to study trace element partitioning between silicate and iron rich liquids at extreme conditions
- Static compression of the 3.65 Å phase of MgSi(OH)<SUB>6</SUB> to 45 GPa
- Surface Modifications of Space-exposed Aerogel from the Stardust Cometary Collector
- Trace elemental nano-imaging of monazite and zircon using synchrotron radiation induced XRF: new insights into polyphase evolution
- In situ insights to Se (S) partitioning between silicate and metallic melts at extreme conditions
- Phase transition in aluminous silica in the lowermost mantle
- Probing Ice Nucleation in "No Man's Land" with Ultrafast X-ray Laser at LCLS
- Silicate-Iron partitioning of Palladium and Ruthemium up to 110 GPa using nano-X-Ray Fluorescence imaging
- Structure of a natural basaltic liquid at mantle pressures up to 59.0 GPa
- Approaches to constrain single-crystal elastic properties from Brillouin scattering of polycrystalline samples
- Cu and Ni solubility in high-temperature aqueous fluids
- Elastic properties and phase transitions of Fe7C3 and new constraints on the light element budget of the Earth's inner core
- Elasticity and thermodynamics of the 3.65 Å phase in subduction zone settings
- Investigation of phase transitions of iron under extreme dynamic compression with XANES measurements at LCLS
- Methane and ethane at high pressures: structure and stability
- Mineralogic reservoirs for high-field strength elements in deeply subducted continental sediments
- Radial X-Ray Diffraction at the Extreme Conditions Beamline of PETRA III: In-Situ Texture Analysis of a Mixture of Perovskite and Ferropericlase to 1100 K and 40 GPa
- Stress- and pressure-induced iron spin-state crossover in lower mantle minerals
- Deformation of (Mg,Fe)O Ferropericlase to Temperatures of 1150 K and Pressures of 96 GPa: Implications for Mantle Flow and Seismic Anisotropy
- First Principles Molecular Dynamics Simulations of Fe-Bearing Melts at High Pressure
- High-pressure, high-temperature deformation of CaGeO<SUB>3</SUB> (perovskite)±MgO aggregates: Elasto-ViscoPlastic Self-Consistent modeling and implications for multi-phase rheology of the lower mantle
- Incorporation of Xenon in magmas at depth
- Melting of iron close to Earth's inner core boundary conditions detected by XANES spectroscopy in laser shock experiment
- The Fate of Subducted Sediment at the Base of the Mantle Transition Zone: Water and the K-hollandite → NAL Phase Transformation
- Trace and Minor Elements in Magmas at High Pressure: In Situ Structural Insights on Partitioning at Depth
- Densification of magmas at depth: geophysical and geochemical consequences
- Equation of state and elasticity of the 3.65 Å phase- constraining mantle hydration from the seismic X-discontinuity
- High-pressure, high-temperature deformation of CaGeO<SUB>3</SUB> (perovskite)±MgO aggregates: Elasto-ViscoPlastic Self-Consistent modeling and implications for multi-phase rheology in the lower mantle
- Structure of carbonate melts at high pressure
- X-ray Raman Scattering at Extreme Conditions: Insights to Local Structure, Oxidation and Spin state
- Iron and iron alloys under laser compression at XFEL for planetary science
- Kinetics Of Bridgmanite To Post-Perovskite Transition in (Mg<SUB>0.85</SUB>,Fe<SUB>0.15</SUB>)SiO<SUB>3</SUB>
- Experimental deformation of (Mg,Fe)O ferropericlase in a resistive-heated DAC at conditions of the Earth's lower mantle
- Geometry and Width of the Ringwoodite - Bridgmanite+Ferropericlase Binary Loop in the System (Mg,Fe)<SUB>2</SUB>SiO<SUB>4</SUB>: Interpretation of the Sharpness of the 660-km Discontinuity
- High pressure study of water-salt systems, phase equilibria, partitioning, thermodynic properties and implication for large icy worlds hydrospheres.
- High-pressure phase transition in silicon carbide under shock loading using ultrafast x-ray diffraction
- Looking for carbonates in the deep Earth: an experimental approach at extreme conditions
- New results of the post-spinel transition pressure in Mg<SUB>2</SUB>SiO<SUB>4</SUB> by means of in-situ X-ray diffraction in a multi-anvil press: complete agreement with the 660-km discontinuity depth
- On the transparency and mechanical durability of nano-polycrystalline ceramics synthesized by high-pressure crystallization from glass
- Pressure-induced amorphization in plagioclase feldspars: A time-resolved powder diffraction study during rapid compression
- Pulsed Laser Techniques to Determine Lattice and Radiative Thermal Conductivity of Deep Planetary Materials at Extreme Pressure-Temperature Conditions
- Solid - solid and solid - liquid phase transitions of iron and iron alloys under laser shock compression
- Tracing iron-carbon redox from surface to core
- Water incorporation in olivine at upper mantle pressures and water-undersaturated conditions
- A Dynamic Diamond Anvil Cell (dDAC) Setup for Time-Resolved High-Temperature X-Ray Diffraction Experiments under Dynamic Compression
- Characterization of the Fe-Si-C system at extreme conditions and its application to carbon-rich exoplanets interior
- Comprehensive equations of state for high pressure ices and aqueous brines for accurate thermodynamic properties predictions.
- Direct Measurements of the Bulk Modulus Softening in (Mg,Fe)O across the Iron Spin Change Measured at Seismic Frequencies in a Dynamic DAC Using Time-Resolved XRD
- Internally resistive heated diamond anvil cell experiments on Fe-Ni-Si alloy to 200 GPa and 3900 K and its implications for Earth's core
- Strain-rate and temperature effects on kinetics of phase transitions in albite
- Texture development and slip system activities of bridgmanite during high temperature deformation of a lower mantle assemblage in a resistively heated diamond anvil cell
- Thermal equation of state of solid Fe3S and its implications for Earth's core
- Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D'' layer
- Melting of Fe<SUB>3</SUB>S under high pressure and the implications for Earth's core
- Partitioning of major and minor elements between melt and solids in the basaltic and peridotitic lithologies at Earth's lower mantle conditions
- Phase relations and melting in a Fe-Si-C core: new constraints from experimental data
- The stability of subducted glaucophane with the Earth's secular cooling
- A Deep Dive into Planetary Abysses: Effects of Pressure, Phase Equilibria and Chemistry on the Structure and Habitability of Icy-Ocean Worlds.
- Bulk modulus of H<SUB>2</SUB>O across the ice VII - ice X transition measured by time-resolved X-ray diffraction in dynamic Diamond Anvil Cell experiments
- Microstructures induced by the post-garnet transformation in mid-ocean ridge basalt (MORB)
- Phase Change of Pyrolitic Material: In-situ Transformation and InducedMicrostructures at 660 km Depth
- Reconciliation of the negative pressure dependence of the 660-km discontinuity depth with the bridgmanite forming reactions in MgO-SiO<SUB>2</SUB> systems
- Revealing chemistry at multi-megabar pressures by means of synchrotron X-ray diffraction: Fe-O system as a case study
- The fate of iron oxides at multimegabar pressure regime
- Atomic-scale mixing between MgO and H2O in the deep interiors of water-rich planets
- Effect of AlAlO3 and MgAlO2.5 incorporation on the equation of state of MgSiO3 bridgmanite
- Enhanced compressibility of ferropericlase across the iron spin crossover at high temperatures, studied by time-resolved X-ray diffraction in a resistively-heated dynamic diamond-anvil cell
- Experimental Investigation of Microstructures at the 660 km Discontinuity
- High-pressure experiments on melting of Fe3C and thermodynamics of the Fe-C system
- Phase Stability and Elasticity of Al-bearing Superhydrous Phase B at High Pressure and Temperature
- The Fe-FeSi Phase Diagram at Mercurys Core Conditions
- The Stishovite to Post-stishovite Phase Transition in Earths Lower Mantle Studied by Time-resolved X-ray Diffraction in a Dynamic Diamond Anvil Cell (dDAC)
- The stability of subducted glaucophane with the Earths secular cooling
- 3D Tomographic Analysis of Volcanic Tephra from the 2020-2022 Activity of Mt. Etna: Insights into Magma Porosity and Crystallinity, and Eruption Style and Intensity
- A tomographic analysis of the melt inclusions of Colli Albani
- Microstructures and Shear Wave Anisotropy in Stishovite: Implications for Mid-Mantle Seismic Heterogeneities
- Multigrain X-ray Diffraction, Data Processing Techniques, and Microstructures in Pyrolite at Lower Mantle Conditions
- Possible link between deeply subducted water and the Eʹ layer
- Recent developments of large-volume multi-anvil technologies for advanced high-pressure-temperature research
- Weak Cubic CaSiO3 Perovskite in Earth's Mantle