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3-D dynamic rupture simulations by a finite volume method
- Source :
- Geophysical Journal International, Geophysical Journal International, Oxford University Press (OUP), 2009, 178 (1), pp.541-560. ⟨10.1111/j.1365-246X.2009.04088.x⟩, Geophysical Journal International, 2009, 178 (1), pp.541-560. ⟨10.1111/j.1365-246X.2009.04088.x⟩, Geophysical Journal International, Oxford University Press (OUP), 2009, 00, pp.000, Geophysical Journal International, 2009, 178 (1), pp.541-560. ⟨10.1111/j.1365-246x.2009.04088.x⟩, Geophysical Journal International, Oxford University Press (OUP), 2009, 178 (1), pp.541-560. ⟨10.1111/j.1365-246x.2009.04088.x⟩
- Publication Year :
- 2009
- Publisher :
- HAL CCSD, 2009.
-
Abstract
- International audience; Dynamic rupture of a 3-D spontaneous crack of arbitrary shape is investigated using a finite volume (FV) approach. The full domain is decomposed in tetrahedra whereas the surface, on which the rupture takes place, is discretized with triangles that are faces of tetrahedra. First of all, the elastodynamic equations are described into a pseudo-conservative form for an easy application of the FV discretization. Explicit boundary conditions are given using criteria based on the conservation of discrete energy through the crack surface. Using a stress-threshold criterion, these conditions specify fluxes through those triangles that have suffered rupture. On these broken surfaces, stress follows a linear slip-weakening law, although other friction laws can be implemented. For The Problem Version 3 of the dynamic-rupture code verification exercise conducted by the SCEC/USGS, numerical solutions on a planar fault exhibit a very high convergence rate and are in good agreement with the reference one provided by a finite difference (FD) technique. For a non-planar fault of parabolic shape, numerical solutions agree satisfactorily well with those obtained with a semi-analytical boundary integral method in terms of shear stress amplitudes, stopping phases arrival times and stress overshoots. Differences between solutions are attributed to the low-order interpolation of the FV approach, whose results are particularly sensitive to the mesh regularity (structured/unstructured). We expect this method, which is well adapted for multiprocessor parallel computing, to be competitive with others for solving large scale dynamic ruptures scenarios of seismic sources in the near future.
- Subjects :
- 010504 meteorology & atmospheric sciences
Discretization
[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]
Geometry
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
010502 geochemistry & geophysics
01 natural sciences
Physics::Geophysics
Geochemistry and Petrology
Numerical approximations and analysis
Shear stress
Boundary value problem
0105 earth and related environmental sciences
Mathematics
Finite volume method
Dynamics and mechanics of faulting
Wave propagation
Mathematical analysis
Finite difference
Body waves
Geophysics
Rate of convergence
[SDU]Sciences of the Universe [physics]
Rheology and friction of fault zones
Tetrahedron
Interpolation
Subjects
Details
- Language :
- English
- ISSN :
- 0956540X and 1365246X
- Database :
- OpenAIRE
- Journal :
- Geophysical Journal International, Geophysical Journal International, Oxford University Press (OUP), 2009, 178 (1), pp.541-560. ⟨10.1111/j.1365-246X.2009.04088.x⟩, Geophysical Journal International, 2009, 178 (1), pp.541-560. ⟨10.1111/j.1365-246X.2009.04088.x⟩, Geophysical Journal International, Oxford University Press (OUP), 2009, 00, pp.000, Geophysical Journal International, 2009, 178 (1), pp.541-560. ⟨10.1111/j.1365-246x.2009.04088.x⟩, Geophysical Journal International, Oxford University Press (OUP), 2009, 178 (1), pp.541-560. ⟨10.1111/j.1365-246x.2009.04088.x⟩
- Accession number :
- edsair.doi.dedup.....ffb94df36f14bc7ca86b82114885beb3
- Full Text :
- https://doi.org/10.1111/j.1365-246X.2009.04088.x⟩