HelioWebUniversity of Munster, Institute for Geophysics
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I[University of Munster, Institute for Geophysics]
PI["Parent Institutions (1)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (102)"]
CA["Linked Collaborating Authors (0)"]
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
- Consequences of a Viscosity Peak in the Lower Mantle for the Evolution of Plumes
- Formation of Plates in Numerical Mantle Convection Models
- Different Tectonic Styles in a Self-Consistent Mantle Convection Model
- Exploring oceanic impact crater mechanics through numerical models
- Synthetic Seismic Signature of Thermal Mantle plumes
- About the Freshwater Contribution of the Eastern Weddell Ice Shelves to Water Mass Formation in the Weddell Sea
- Coupled Ice Shelf -- Ocean System Simulations for Different Climate Scenarios
- Stability of Antarctic Ice Shelves and Their Role in the Global Climate System
- Surface Tectonics and Internal Dynamics of Mars
- Using Subdivision Surfaces and Adaptive Surface Simplification Algorithms for Modeling Chemical Heterogeneities in Geophysical Flows
- Temporal Variations in the Convective Style of Planetary Mantles
- The Chemical Surface Signature Created by Upwelling Plumes
- The Dynamics of Layer Formation in the Earth's Mantle
- Thermal convection in a 3D spherical shell with strongly temperature and pressure dependent viscosity
- A Numerical Study on Possible Driving Mechanisms of Core Convection
- Dynamical Generation of the Transition Zone in the Earth's Mantle
- Dynamics of Metal-Silicate Separation in a Terrestrial Magma Ocean
- Low Viscosity Zone and Mantle Dynamics
- Spatial and Temporal Variability in Active Layer Thickness over the Russian Arctic Drainage Basin
- Temporal Variations in the Convective Style of Planetary Mantles
- Variable Quality Compression of Fluid Dynamical Data Sets Using a 3D DCT Technique
- Bedrock topography beneath the temperate ice cap on King George Island, Antarctica as derived from numerical simulations applying different basal sliding laws
- Dynamical Generation of a Bumpy Layer at the Core-Mantle-Boundary
- Dynamics and Mass Balance of Riiser-Larsen Ice Shelf, Antarctica, and its Drainage Area
- Scenarios of Future Water use on Mediterranean Islands based on an Integrated Assessment of Water Management
- Temporal Variations in the Convective Style of Planetary Mantles
- Trends in Simulated and Observed Active Layer Depth Over the Arctic Drainage Basin and the Tibetan Plateau
- Freezing of a Magma Ocean and Subsequent Mantle Differentiation
- Plate Motions and the Viscosity Structure of the Mantle
- Temporally Transitional Mantle Convection: Implications for Mars
- The Effect of Subduction Events on Rising Mantle Currents
- Boundary Layer Control of Rotating Convection Systems
- Dynamic Mechanisms Behind Periodic and Episodic Phenomena in the Earth's Interior
- Numerical Mantle Convection Modeling: The Effect of Plates on the Surface Topography
- Detection and Absence of Ultra Low Velocity Zones (Invited)
- Dynamic Layer Formation in Planetary Interiors
- Evidence for Hot Material Subducted beneath the Kurile Slab
- Is the D" reflector a phase transition? (Invited)
- Spontaneous Layer Formation in Salt Fingering Simulations
- The effect of internal heating on plate dynamics in planetary mantle convection
- Fe-bearing perovskite and post-perovskite: phase stability, spin transitions, and the consequences for the lower mantle
- Numerical Study on plumes and thermochemical piles in plate-mode convection
- P-wave attenuation tomography of Mount St. Helens: preliminary results from coda-normalized spectra
- Thermal Structure and Lithospheric Mobility of Super-Earths
- Turbulent Convection in the Zero Reynolds Number Limit (Invited)
- 3D simulations of double-diffusive convection in the interior of giant planets
- Deep mantle structure in the vicinity of the Tethys slab using a seismic array in Morocco
- Double Diffusive Layering In The Early Earth's Mantle- Consequences For Thermal History And Surface Dynamics
- Influence of rotation on iron particles in an early magma ocean
- Lower Mantle Scattering Observations at Temporary Arrays
- Numerical Simulation of Large-Scale Double-Diffusive Systems
- Numerical study on double-diffusive convection in the Earth's core
- The effect of mantle internal heating and pressure-weakening on surface dynamics: implications for Super-Earths
- The lowermost mantle beneath Bering Sea
- Are Strong Zonal Winds in Giant Planets Caused by Density-Stratification?
- Numerical Parameter Study of the Rotational Influence on the 'Metal Rain Scenario'
- On the Possibility of a Thin, Molten Silicate Basal Magma Layer at the Base of Earth's Mantle
- Ambient seismic noise levels: A survey of the permanent and temporary seismographic networks in Morocco, North Africa
- Array analysis of S and ScS waveforms for Pacific lowermost mantle structure
- Crystal settling and crystal growth caused by Ostwald Ripening in a terrestrial magma ocean under rotation
- Extreme rotating convection experiments and implications for modeling the dynamo
- From 2d to 3d Attenuation Tomography in Deception Island (antarctica)
- On the origin of the D'' discontinuity: Combining seismological observations with mineral physics
- Precessionally driven dynamos in ellipsoidal geometry
- The Effect of Compositional Variations in the Mantle on Surface Mobility
- The Onset of Plate tectonics in a Compositionally Stratified mantle
- Tomography of the upper mantle beneath the African/Iberian collision zone
- Effects of Rotation on the Differentiation of a terrestrial Magma Ocean
- The Selfconsistent Evolution of Thermochemical Boundary Layers in the Earth's Mantle
- Effects of rotation on crystal settling in a terrestrial magma ocean: Spherical shell model
- Impact of Rotation on the Differentiation of a Terrestrial Magma Ocean
- The Layered Nature of Planetary Mantle
- Chemical Transport Across The Core-Mantle Boundary- Impact On The Formation Of A Bumpy Layer
- On the effects of planetary rotation on the differentiation of a terrestrial magma ocean in spherical geometry
- Constraining the Mechanism of D" Anisotropy: Diversity of Observation Types Required
- Electrical resistivity structure beneath the Hangai Dome, Mongolia: intraplate volcanism and deformation imaged with magnetotelluric data
- On the effects of planetary rotation on early Earth differentiation
- Self-Organized Mantle Layering After the Magma-Ocean Period
- The DESMEX Project - Deep Electromagnetic Sounding for Mineral EXploration
- Double Diffusive Convection - Creating Boundary Layers within the Earth's Mantle
- Layer formation in Europa's subsurface ocean by double-diffusive convection
- Modeling and Observations of Seismic Anisotropy in the Lowermost Mantle Beneath Siberia
- Modeling the Dynamics of Magma Ocean Solidification
- On the evolution of metal delivered by giant impacts in a convecting and rotating magma ocean
- Scattering shades across Southern Morocco: what coda and body waves constrains can tell about Multiscale Heterogeneous structures.
- The Influence of a Compositionally Distinct Layer in the Deep Mantle on the Evolution of Plate-like Surface Motion
- Formation of cellular structures on Sputnik Planitia from convection
- How long can layers last in the subsurface oceans of icy satellites?
- Intra-continental uplift and volcanism in the Hangai and Gobi-Altai Mountains in Mongolia; Insights from a magnetotelluric multiscale 3-D inversion
- Kinetics and detectability of the bridgmanite to post-perovskite transformation in the Earth's D'' layer
- Modeling of lowermost mantle anisotropy with multiple data types: Case studies beneath Siberia and the Indian Ocean
- Probing mantle plumes using seismic arrays
- Self-Consistent Formation of Piles by a Diffusive Influx From the Core
- Separate regime transitions for heat and momentum transport in laboratory-numerical models of planetary core convection
- The DESMEX System: Novel Developments for Semi-Airborne Electromagnetic Exploration
- The Signal of Outermost Core Stratification in Body Wave and Normal Mode Data
- A "strange phase" in PP precursor
- A new look at polarity information in D" reflections
- Dehydration Melting Below the Undersaturated Transition Zone and Implications for Mantle Water Content
- New insights on the interaction between seismic waves and mantle plumes
- Olivine to Wadlseyite Transformation in (Mg,Fe)<SUB>2</SUB>SiO<SUB>4</SUB> and the 410 km Depth Discontinuity : Experiments and Models
- Strong Topography of the Mid-Mantle Reflector Beneath the Northern Atlantic