The deal. II library, version 9.2
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The deal. II library, version 9.4
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The deal. II library, version 9.0
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The deal. II library, version 9.3
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High accuracy mantle convection simulation through modern numerical methods–II: realistic models and problems
Computations have helped elucidate the dynamics of Earth's mantle for several decades
already. The numerical methods that underlie these simulations have greatly evolved within …
already. The numerical methods that underlie these simulations have greatly evolved within …
Coupled influence of tectonics, climate, and surface processes on landscape evolution in southwestern North America
The Cenozoic landscape evolution in southwestern North America is ascribed to crustal
isostasy, dynamic topography, or lithosphere tectonics, but their relative contributions remain …
isostasy, dynamic topography, or lithosphere tectonics, but their relative contributions remain …
101 geodynamic modelling: How to design, carry out, and interpret numerical studies
Geodynamic modelling provides a powerful tool to investigate processes in the Earth's crust,
mantle, and core that are not directly observable. However, numerical models are inherently …
mantle, and core that are not directly observable. However, numerical models are inherently …
Nonlinear viscoplasticity in ASPECT: benchmarking and applications to subduction
ASPECT (Advanced Solver for Problems in Earth's ConvecTion) is a massively parallel finite
element code originally designed for modeling thermal convection in the mantle with a …
element code originally designed for modeling thermal convection in the mantle with a …
Victoria continental microplate dynamics controlled by the lithospheric strength distribution of the East African Rift
The Victoria microplate between the Eastern and Western Branches of the East African Rift
System is one of the largest continental microplates on Earth. In striking contrast to its …
System is one of the largest continental microplates on Earth. In striking contrast to its …
Evolution of rift systems and their fault networks in response to surface processes
Continental rifting is responsible for the generation of major sedimentary basins, both during
rift inception and during the formation of rifted continental margins. Geophysical and field …
rift inception and during the formation of rifted continental margins. Geophysical and field …