Tag: feature:cartesian#
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- Advection stabilization benchmarks
- The Blankenbach convection benchmark
- Buiter et al. 2008, JGR
- Brittle thrust wedges benchmark
- The Burstedde variable viscosity benchmark
- Compressibility formulation benchmarks
- The Crameri et al. benchmarks
- Diffusion of Hill
- Donea & Huerta 2D box geometry benchmark
- Entropy adiabat benchmark
- Finite strain benchmark
- Viscoelastic half-space loading
- Viscous half-space loading
- Grain Size Pinned State
- The “inclusion” Stokes benchmark
- 2D Lithosphere flexure benchmark with infill
- The King compressible convection benchmark
- Layered flow with viscosity contrast
- Newton Solver Benchmark Set - Nonlinear Channel Flow
- Newton Solver Benchmark Set - Spiegelman et at. (2016)
- Newton Solver Benchmark Set - Tosi et at. (2015)
- The NSinker benchmark
- Onset of convection benchmark
- Benchmarks for operator splitting
- Particle distribution benchmark
- Particle integration scheme benchmark
- Polydiapirism
- The Rayleigh-Taylor instability
- The Rayleigh-Taylor instability with a free surface
- The rigid shear benchmark
- Magmatic shear bands
- The sinking block benchmark
- The slab detachment benchmark
- The SolCx Stokes benchmark
- The solitary wave benchmark
- The SolKz Stokes benchmark
- 1D test for water solubility
- Tan & Gurnis, 2007
- The Tosi et al. benchmarks
- The bending beam benchmark
- Visco(elastic)-plastic shear bands after Gerya (2019)
- The viscoelastplastic shear bands benchmark
- The viscoelastoplastic simple shear benchmark
- Viscoelastic plate flexure
- The viscoelastic relaxation benchmark
- The viscoelastic sheared torsion benchmark
- The viscoelastic stress build-up benchmark
- Viscosity grooves benchmark
- Yamauchi & Takei anelastic shear wave velocity-temperature conversion benchmark
- Zhong et al., 1993
- CPO induced anisotropic viscosity
- Rift interaction in brittle-ductile coupled systems
- Anisotropic viscosity
- Convection in a 2d box with a phase transition
- The active case with reactions.
- The active case.
- Using active particles.
- The passive case.
- The passive case with particles
- Continental extension
- Running a geodynamic model
- Convection in a 2d box
- Convection in a 3d box
- Crustal deformation
- Olivine Fabric Developments Under Simple Shear
- Fastscape Eroding Box
- Tracking finite strain
- Using a free surface
- Using a free surface in a model with a crust
- Reading in compositional initial composition files generated with geomIO
- Melt migration in a 2D mantle convection model
- Sublithospheric convection beneath an oceanic plate with a grain size dependent rheology
- Convective and conductive heat flow: Cooling of oceanic lithosphere
- Viscous inclusions under simple and pure shear
- Kinematically-driven 2d oceanic subduction
- Latent heat benchmark
- Lower crust flow with an obstacle
- Magnetic lineations on the sea floor
- Melt migration in a 2D mid-ocean ridge model
- Reproducing rheology of Morency and Doin, 2004
- Using lazy expression syntax for if-else-statements in function expressions
- Onset of convection
- Using Non-Equilibrium Thermodynamics to Drive Phase Transformations
- Convection in a box with prescribed, variable velocity boundary conditions
- Prescribed internal velocity constraints
- Prescribing internal velocity constraints with ASCII files
- Averaging material properties
- Sinking of anhydrite blocks within a Newtonian salt diapir
- The “Stokes’ law” benchmark
- Subduction initiation from Matsumoto and Tomoda (1983)
- Simplified Subduction Model with Parameterized Solid-Fluid Reactions
- Using the World Builder to model the thermal structure of oceanic transform faults
- Computation of the van Keken Problem with the Volume-of-Fluid Interface Tracking Method
- The van Keken thermochemical composition benchmark
- Van Keken 2008 corner flow recreation
- Visualizing phase diagrams
