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Neural network emulators for geodynamics: for uncertainties, sensitivity and the impatient |
| Bower et al. |
Evolution of terrestrial planets from molten to solid |
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Tectonic predictions with mantle convection models |
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Abrupt upper-plate tilting during slab transition-zone collision |
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Intra-plate volcanism: the role of plumes, plate motion, plate motion changes and lithospheric structure |
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Interpreting continental break-up from surface observations: analysis of 1D partial melting using synthetic waveform propagation |
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Towards ASPECT 2.0: Features and software structure |
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3D instantaneous dynamics modeling of present-day Aegean subduction |
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Magmatism by delamination: Bimodal melting patterns inferred by numerical models |
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Layer-formation in the early Earth’s mantle |
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Impact of the overriding plate rheology on convergence zone dynamics |
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The dynamics of Adria: a unique complexity unraveled in laboratory models |
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Timing and distribution of magmatism at magma-poor margins: Controls from crustal rheology and depleted cratonic lithosphere |
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Non-thermal equilibrium two-phase flow for melt migration and ascent |
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Constraining upper mantle viscosity and plate boundary friction using global plate motions and lithosphere net rotation |
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Initiation of subduction by small scale convection: new insights from viscoelastic models with a free surface |
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Analogue modelling of opposite subduction retreating in adjacent plates |
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The effect of oblique convergence on temperature in subduction zones: insights from 3D numerical modelling |
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Physical and numerical ingredients of a 3D continuum seismic cycle code |
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Formation and stability of a double subduction system: a numerical study |
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Understanding the Yellowstone magmatic system using geodynamic simulations |
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Dynamic modelling of Venus interior evolution and implications for mantle viscosity structure and surface observables |
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The effect of regularisation in global tomography on mantle density models |
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A coupled petrological-geodynamical model to investigate the evolution of crustal magmatic systems |
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Thermo-mechanical two-phase flow models of magma ascent in the continental crust: effect of heat flow and extension |
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3D dynamics of crustal deformation along the western Andean margin |
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Fault reactivation due to glacially induced stresses |
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A computational framework to optimise global absolute plate motion models |
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Deformation, crystal preferred orientations, and seismic anisotropy in the Earths D” layer |
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Sequential data assimilation for solid Earth sciences: Probabilistic estimation and forecasting of fault stresses |
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Melting and melt flow under continental crust conditions: numerical ex- ploration of flow rheologies of melt and rock |
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The energetics of evolving convective systems: Internal heating, mixing, and Earth’s evolution |
| Zhou et al. |
Subduction initiation propagates along the transform fault: 3D numerical modeling |
