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A Domain Decomposition Approach to Implementing Fault Slip in Finite-Element Models of Quasi-static and Dynamic Crustal Deformation

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TLDR
In this article, a domain decomposition approach with Lagrange multipliers is employed to implement fault slip in a finite-element code, PyLith, for use in both quasi-static and dynamic crustal deformation applications.
Abstract
We employ a domain decomposition approach with Lagrange multipliers to implement fault slip in a finite-element code, PyLith, for use in both quasi-static and dynamic crustal deformation applications. This integrated approach to solving both quasi-static and dynamic simulations leverages common finite-element data structures and implementations of various boundary conditions, discretization schemes, and bulk and fault rheologies. We have developed a custom preconditioner for the Lagrange multiplier portion of the system of equations that provides excellent scalability with problem size compared to conventional additive Schwarz methods. We demonstrate application of this approach using benchmarks for both quasi-static viscoelastic deformation and dynamic spontaneous rupture propagation that verify the numerical implementation in PyLith.

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Coupled multiphase flow and poromechanics: A computational model of pore pressure effects on fault slip and earthquake triggering

TL;DR: In this article, the authors presented a new computational approach to model coupled multiphase flow and geomechanics of faulted reservoirs, where faults were modeled as surfaces embedded in a three-dimensional medium by using zero-thickness interface elements to accurately model fault slip under dynamically evolving fluid pressure and fault strength.
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Green’s functions for geophysics: a review

TL;DR: This article provides a relatively complete review on GFs for geophysics, which can be scaled and applied to large- scale problems such as those involved in Earth sciences as well as to nano-scale problems associated with quantum nanostructures.
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Revisiting viscoelastic effects on interseismic deformation and locking degree: A case study of the Peru‐North Chile subduction zone

TL;DR: In this paper, the authors use finite element method (FEM) models to investigate the control of viscoelasticity on interseismic deformation and to highlight the pitfalls of interpreting the data with purely elastic models for both the forward and inverse problems.
References
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TL;DR: In this article, the construction of a finite element of space in Sobolev spaces has been studied in the context of operator-interpolation theory in n-dimensional variational problems.
Journal ArticleDOI

Tectonic stress and the spectra of seismic shear waves from earthquakes

TL;DR: In this paper, an earthquake model is derived by considering the effective stress available to accelerate the sides of the fault, and the model describes near and far-field displacement-time functions and spectra and includes the effect of fractional stress drop.
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