Bolrao |
Numerical simulations of melting-crystallisation processes at the boundaries between magma oceans and solid mantle |
Boonma |
Dependence of slab buoyancy on composition and convergence rate: insights from kinematic modelling |
Bredow et al. |
Variable melt production rate of the Kerguelen hotspot due to long-term plume-ridge interaction |
Buiter & Shephard |
Numerical experiments investigating alternative extension velocity histories for the North Atlantic rifted margins |
Chotalia et al. |
Water, viscosity and mantle convection: the effects of weakening and mixing |
Ciskova & Bina |
Rheological effects on slab stagnation in the transition zone and uppermost lower mantle |
Conrad et al. |
Volumes and patterns of asthenospheric melt inferred from the space-time distribution of seamounts |
Costa et al. |
Numerical modeling of large-scale lateral collapses in volcanic edifices |
Crameri |
StagLab: Post-processing and visualizing mantle and lithosphere dynamics |
Dal Zilio et al. |
Under the hood of the earthquake machine: Toward predictive modeling of the Himalayan seismic cycle |
Dannberg & Gassmoeller |
Chemical trends in ocean islands explained by plume–slab interaction |
Davaille et al. |
Plume-induced subduction and accretion on convecting planets: experiments and scaling relationships |
Dohmen & Schmeling |
Modeling of solitary porosity waves with new viscosity laws |
Eichheimer et al. |
Towards modelling of water inflow into the mantle |
Ficini et al. |
Mantle convection: clues from lithosphere sinking at subduction zones |
Fraters et al. |
Efficient and practical Newton solvers for nonlinear Stokes systems in geodynamic problems |
Fuchs & Becker |
Plate like convection with viscous strain weakening and corresponding surface deformation pattern |
Gerardi & Rice |
Boundary-element modeling of two-plate interaction at subduction zones: scaling laws and a geophysical constraint |
Glerum et al. |
3D Numerical rift modeling with an application to the East African Rift System |
Golabek et al. |
Post-magma ocean mixing of reservoirs inside the angrite parent body |
Grima et al. |
The slab-mantle interaction, deformation and its translated surface topography effects |
Guelcher et al. |
Influence of detachment faults on intra-oceanic subduction initiation: 3D thermomechanical modelling |
Hellenkamp et al. |
The influence of internal heat sources on mantle convection with phase transitions |
Houser et al. |
Life on a dry Planet |
Humphreys et al. |
Recent craton growth by slab stacking beneath Wyoming |
Jain et al. |
Self-consistent generation of primordial continental crust in global mantle convection models |
Jimenez-Munt et al. |
Geodynamic model of recent deformation in central Eurasia |
Jimenez-Diaz |
Mechanical characterization of the Eastern Central Atlantic hotspots |
Kaus et al. |
Regularized non-local plasticity models for geodynamic simulations |
Liu et al. |
The influence of the orogenic lithospheric strength on foreland deformation patterns |
Long & Ballmer |
Intraplate volcanism in northeast China due to upwellings rising from the stagnant slab |
Magni et al. |
Continental underplating after slab break-off |
Mameri et al. |
Mechanical anisotropy in the upper mantle: a comparison between ex- perimental observations and model predictions |
Manjon-Cabeza Cordoba & Ballmer |
Edge-driven convection: Geodynamic modelling and implications for volcanism |
Mittelstaedt and Davaille |
Controls on the formation and evolution of microplates in scaled laboratory experiments |
Raess et al. |
Localised two-phase flow: Application of implicit matrix-free pseudotransient method |
Rüpke |
Deformation, fluid flow and mantle serpentinization at oceanic transform faults |
Sibrant et al. |
Role of axial strength of the lithosphere on the accretion mode of mid-ocean ridges |
Stein and Hansen |
The presence of dense material in the deep mantle: implications for plate motion |
Willis et al. |
The Altyn Tagh fault: quantifying the contribution of strain-weakening on lithospheric rheology |
Wong et al. |
Lithospheric stresses on Europa’s icy shell: Can subduction initiate on Europa? |