Robust characteristics method for modelling multiphase visco-elasto-plastic thermo-mechanical problems
By Taras V. Gerya, D. Yuen. 2007
469 citations recorded by the source corpus.
Subfields: Geophysics, Molecular Biology
View Paper: https://www.semanticscholar.org/paper/49a148c3c9202f0871404d460e8ad93c5c50112b
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In Geophysics
In Molecular Biology
Citations in the corpus
- Numerical modelling of magma dynamics coupled to tectonic deformation of lithosphere and crust (2013, methodology): “…as we will show, represents a straightforward extension of the standard formulation of Stokes flow used in many geodynamic simulations of mantle or lithosphere deformation today (Moresi et al. 2003; Gerya & Yuen 2007; Kaus et al. 2008; May & Moresi 2008; Popov & Sobolev 2008; Kaus 2010).”
- Transient hot channels: Perpetrating and regurgitating ultrahigh-pressure, high-temperature crust–mantle associations in collision belts (2008, methodology): “The code was tested for a variety of problems by comparing results with both analytical solutions (Gerya and Yuen, 2003a; Gerya and Yuen, 2007) and analogue sandbox experiments (Buiter et al.”
- Why is terrestrial subduction one-sided? (2008, methodology): “D) with the use of the code I2ELVIS (Gerya and Yuen, 2007) based on fi nite-differences and marker-in-cell technique.”
- Subduction styles in the Precambrian: Insight from numerical experiments (2009, methodology): “The 2D continuity equation with time-dependent density describes the conservation of mass for a compressible fluid (Gerya and Yuen, 2007), as follows, Aυx Ax + Aυz Az = − 1 ρ Dρ Dt ; ð18Þ where DρDt is the substantive density time derivative which accounts locally for melt extraction.”
- Three-dimensional thermomechanical modeling of oceanic spreading initiation and evolution (2013, unknown): “The momentum, mass and heat conservation equations are solved with the thermomechanical code I3ELVIS (Gerya and Yuen, 2007) on the non-deforming Eulerian grid whereas the advection of transport properties including viscosity, plastic strain, temperature etc. is performed by advecting the Lagrangian…”
- Driving the upper plate surface deformation by slab rollback and mantle flow (2014, methodology): “Surface processes are implemented using a highly simplified gross-scale erosion–sedimentation law according to which instantaneous erosion limits mountains height to 4 km above the reference water level (y = 12 km), whereas instantaneous sedimentation limits trench depth to 8 km below the water leve”
- Subduction initiation at passive margins: Numerical modeling (2010, background): “continental crust over the oceanic one and related viscoplastic bending of the oceanic plate [ Gerya and Yuen, 2007; Faccenda et al., 2008].”