Comments (1)
closing because this would be a significant change to the code base. Perhaps for future.
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Related Issues (20)
- Coupled Evolution of Deformation, Pore Fluid Pressure, and Fluid Flow in the thrust-fold mountain belt ? HOT 4
- Uncoupled temperature and compositional field in UW Geodynamics HOT 2
- Adding two plasticities to one material HOT 3
- SystemError: <built-in function SystemLinearEquations_UpdateSolutionOntoNodes> returned a result with an exception set HOT 1
- Parallel computing and An installation problem (MpiRun) HOT 4
- 'surface' integration HOT 2
- Model.mesh.deform_mesh() error with mpirun. Possibly two nodes are in an identical location.
- Installation error HOT 11
- Compressible mantle convection with tala approximation HOT 1
- A question about strata results from coupled model HOT 3
- May I ask how is the second-order invariant of strain rate(function: fn.tensor.second_invariant)in underworld2.13 calculated?
- Question about using mesh.specialSets['MinI_VertexSet'] as a boundary index with parallel run
- Converging issue for 3D subduction model with oblique trench shape. HOT 1
- May I ask how to use Underworld2 modeling the melt-related process?
- An issue when using trapezoid mesh HOT 1
- issue with surface processes
- To find the example to generate collision_wedge.gif HOT 2
- running time HOT 4
- Update the conda channel version and installation tutorial
- Position matching error between the order of saving Passive Tracers and the order of initial Passive Tracers HOT 3
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