Published June 2, 2023
| Version v1
Dataset
Open
Ptatin2D : dataset for run simulations presented in the article Slab pull driven South China Sea opening implies a Mesozoic Proto South China Sea
Authors/Creators
- 1. × Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, UC San Diego, La Jolla, CA, USA
- 2. Sorbonne Université
Description
Overview of pTatin2D
pTatin2D is a software package designed for studying long time-scale processes relevant to geodynamics. The original motivation for this development was to provide the community with an open-source toolkit capable of studying high-resolution, two-dimensional models of lithospheric deformation.
Functionality
- mixed finite elements (Q2-P1_disc) for the Stokes problem
- material points for tracking Lagrangian state and history variables
- energy equation solved with Q1 elements + SUPG
- ALE formulations (with a variety of remeshing solutions)
- extensible rheology components (currently supports: iso-viscous, Frank-Kamenetskii, Arrhenius, power-law, von Mises, Drucker Prager)
- full support for spatio-temporal Dirichlet and non-zero Neumann boundary conditions
- coupling with landscape evolution models
- full support for Newton and Picard non-linear solvers
- massively parallel implementation
pTatin2D leverages functionality from PETSc
Requirements
- PETSc (only support for version 3.2)
Files
densmaps.zip
Files
(569.4 MB)
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Additional details
References
- Larvet et al. (2022) Cimmerian block detachment from Gondwana: A slab pull origin? https://doi.org/10.1016/j.epsl.2022.117790
- May et al. (2015) A scalable, matrix-free multigrid preconditioner for finite element discretizations of heterogeneous Stokes flow https://doi.org/10.1016/j.cma.2015.03.014