about
Mars environment and magnetic orbiter scientific and measurement objectives.PLANET TOPERS: Planets, Tracing the Transfer, Origin, Preservation, and Evolution of their ReservoirS.Water, Life, and Planetary Geodynamical EvolutionModelling the internal structure of Ceres: Coupling of accretion with compaction by creep and implications for the water-rock differentiationSheet-like and plume-like thermal flow in a spherical convection experiment performed under microgravityEstimating precipitation on early Mars using a radiative-convective model of the atmosphere and comparison with inferred runoff from geomorphologyThe Lavoisier mission : A system of descent probe and balloon flotilla for geochemical investigation of the deep atmosphere and surface of VenusPresent-Day Mars' Seismicity Predicted From 3-D Thermal Evolution Models of Interior DynamicsOnset of solid-state mantle convection and mixing during magma ocean solidificationThe habitability of a stagnant-lid EarthA review of volatiles in the Martian interiorHow large are present-day heat flux variations across the surface of Mars?Large Scale Numerical Simulations of Planetary InteriorsWater in the Martian interior-The geodynamical perspectiveMercury's low-degree geoid and topography controlled by insolation-driven elastic deformationThermal evolution and Urey ratio of MarsThermo-Chemical Mantle Convection Simulations Using GaiaA long-lived lunar dynamo powered by core crystallizationCan a fractionally crystallized magma ocean explain the thermo-chemical evolution of Mars?The tectonic mode of rocky planets: Part 1 – Driving factors, models & parametersAsymmetric thermal evolution of the MoonLong-Term Evolution of the Martian Crust-Mantle SystemMagma Ocean Cumulate Overturn and Its Implications for the Thermo-chemical Evolution of MarsOutgassing History and Escape of the Martian Atmosphere and Water InventoryOverturn and evolution of a crystallized magma ocean: A numerical parameter study for MarsThermochemical evolution of Mercury's interiorFuture Mars geophysical observatories for understanding its internal structure, rotation, and evolutionThe influence of pressure-dependent viscosity on the thermal evolution of super-earthsThermal and transport properties of mantle rock at high pressure: Applications to super-EarthsThermo-chemical evolution and global contraction of mercuryVolcanic outgassing of CO2 and H2O on MarsGeophysical and Atmospheric Evolution of Habitable PlanetsMars environment and magnetic orbiter model payloadA Comparative Study of the Influence of the Active Young Sun on the Early Atmospheres of Earth, Venus, and MarsAn alternative mechanism for recent volcanism on MarsPlanetary Magnetic Dynamo Effect on Atmospheric Protection of Early Earth and MarsCorrection to “Influence of a variable thermal conductivity on the thermochemical evolution of Mars”Influence of a variable thermal conductivity on the thermochemical evolution of MarsQ57662535Overturn of Ilmenite‐Bearing Cumulates in a Rheologically Weak Lunar Mantle
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P50
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Duits onderzoekster
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researcher
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հետազոտող
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D. Breuer
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D. Breuer
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D. Breuer
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Doris Breuer
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Doris Breuer
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Doris Breuer
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D. Breuer
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D. Breuer
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Doris Breuer
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Doris Breuer
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P106
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