BR
Publications
- Benchmark forward gravity schemes: the gravity field of a realistic lithosphere model WINTERC-G
- The interior-atmosphere coupling of rocky worlds
- The use of Non-Linear Geometry (NLGEOM) and gravity loading in flat and spherical Finite Element models of Abaqus for Glacial Isostatic Adjustment (GIA)
- Benchmark forward gravity schemes: the gravity field of a realistic lithosphere model WINTERC-G
- Combining the deep Earth and lithospheric gravity field to study the density structure of the upper mantle
- Supplementary material to "Benchmark forward gravity schemes: the gravity field of a realistic lithosphere model WINTERC-G"
- A re-analysis of the lithospheric flexure on Mars
- Is the lithospheric flexure strong enough to hold up the Tharsis Rise? A re-analysis of flexure on Mars
- Asteroid Gravity-Field Estimation
- MaQuIs - Mars Quantum Gravity Mission
- The changing gravity field due to a superplume under the Tharsis Region
- Rocky worlds: What do a planet's orbital parameters tell us about its mantle state?
- Inversion of the lateral density variations of the lithosphere using the full gravity gradient tensor
- Simulating horizontal crustal motions of glacial isostatic adjustment using compressible Cartesian models
- The global gravity field of Mars reveals an active interior
- Sensitivity analysis on gravity change data in order to observe mantle convection
- Present-day surface heat flux variations on the Moon from global geodynamic and crustal thickness models
- Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field
- Glacial isostatic adjustment on Mars
- Satellite gravity-rate observations to uncover Martian plume-lithosphere dynamics
- The present-day surface heat flux of the Moon from global geodynamic and crustal thickness models.
- GRACE and GRACE-FO constraints on 3D GIA models
- GRACE constraints on Earth rheology of the Barents Sea and Fennoscandia
- GRACE constraints on Earth rheology of the Barents Sea and Fennoscandia
- Glacial isostatic adjustment reveals Mars’s interior viscosity structure
- Constraining the distribution of radiogenics on the Moon from global geodynamic models
- Geodynamic modelling the thermochemical structure of the Earth's mantle using integrated geophysical and petrological inversion of surface wave and satellite gravity data
- 3D Lithospheric-scale thermal model of central and southern California
- Benchmarking dynamic topography across geodynamical codes
- Exploring the origin of lunar magnetic anomalies through the Parker Inversion method
- Application of Satellite Gravimetry and AI to Map the Density Distributions of Mars’s Upper Layers