Particle-in-cell | M@TE

4 posts tagged with “Particle-in-cell”

Mantle flow and upper plate deformation due to slab step

Mantle flow and upper plate deformation due to slab step

Subduction dynamics and plate coupling along seismically active margin: the role of slab steps

Uploaded by: Thyagarajulu Gollapalli

Uploaded: October 24, 2024

Software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud

Tags:

Finite element Particle-in-cell Plate boundary Python Subduction

Marker lines prior to (a) and after 750 years of flow of (b) isotropic and (c) anisotropic ice. The axial plane of the resulting shear fold in isotropic ice mimics the bedrock topography, while it is controlled by shearing along a horizontal shear zone in the case of anisotropic ice. Green: bedrock, flow to the right.

Marker lines prior to (a) and after 750 years of flow of (b) isotropic and (c) anisotropic ice. The axial plane of the resulting shear fold in isotropic ice mimics the bedrock topography, while it is controlled by shearing along a horizontal shear zone in the case of anisotropic ice. Green: bedrock, flow to the right.

ISMIP-HOM benchmark experiments using Underworld

Uploaded by: Dan Sandiford

Uploaded: August 19, 2024

Software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud

Tags:

Finite-Element Particle-in-cell Python Stokes anisotropy benchmark ice-sheet mechanical

Figure 5. Evolution of the stress at the reference point (0, 0, −10 km) (a), maximum slip rate along the entire fault zone (b)
and the adaptive time step used in simulation (c) for the reference model.

Figure 5. Evolution of the stress at the reference point (0, 0, −10 km) (a), maximum slip rate along the entire fault zone (b)
and the adaptive time step used in simulation (c) for the reference model.

Numerical Modeling of Earthquake Cycles Based On Navier-Stokes Equations With Viscoelastic-Plasticity Rheology

Uploaded by: Haibin Yang

Uploaded: August 16, 2024

Software: Underworld

Tags:

Cratonic Earthquakes Earthquake Cycles Finite element Navier-Stokes Particle-in-cell Python Viscoelastic-Plasticity

Stress evolution of more buoyant arc-continent collision. This style of collision results in slab break-off

Stress evolution of more buoyant arc-continent collision. This style of collision results in slab break-off

The Role of Lithospheric-Deep Mantle Interactions on the Style and Stress Evolution of Arc-Continent Collision

Uploaded by: Andres Felipe Rodriguez Corcho

Uploaded: May 24, 2024

Software: Underworld2

Tags:

Finite Element MPI Particle-in-cell Python arc-collision buoyancy contrast gravitational collapse slab-anchoring slab-folding

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