Pelties et al., 2012 - Google Patents
Three‐dimensional dynamic rupture simulation with a high‐order discontinuous Galerkin method on unstructured tetrahedral meshesPelties et al., 2012
View PDF- Document ID
- 5047320121415225757
- Author
- Pelties C
- De la Puente J
- Ampuero J
- Brietzke G
- Käser M
- Publication year
- Publication venue
- Journal of Geophysical Research: Solid Earth
External Links
Snippet
Accurate and efficient numerical methods to simulate dynamic earthquake rupture and wave propagation in complex media and complex fault geometries are needed to address fundamental questions in earthquake dynamics, to integrate seismic and geodetic data into …
- 238000004088 simulation 0 title description 22
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. analysis, for interpretation, for correction
- G01V1/282—Application of seismic models, synthetic seismograms
-
- G—PHYSICS
- G06—COMPUTING; CALCULATING; COUNTING
- G06F—ELECTRICAL DIGITAL DATA PROCESSING
- G06F17/00—Digital computing or data processing equipment or methods, specially adapted for specific functions
- G06F17/50—Computer-aided design
- G06F17/5009—Computer-aided design using simulation
- G06F17/5018—Computer-aided design using simulation using finite difference methods or finite element methods
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/60—Analysis
- G01V2210/67—Wave propagation modeling
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/16—Receiving elements for seismic signals; Arrangements or adaptations of receiving elements
- G01V1/18—Receiving elements, e.g. seismometer, geophone or torque detectors, for localised single point measurements
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/60—Analysis
- G01V2210/61—Analysis by combining or comparing a seismic data set with other data
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/003—Seismic data acquisition in general, e.g. survey design
- G01V1/005—Seismic data acquisition in general, e.g. survey design with exploration systems emitting special signals, e.g. frequency swept signals, pulse sequences or slip sweep arrangements
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V99/00—Subject matter not provided for in other groups of this subclass
- G01V99/005—Geomodels or geomodelling, not related to particular measurements
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/008—Earthquake measurement or prediction
-
- G—PHYSICS
- G06—COMPUTING; CALCULATING; COUNTING
- G06F—ELECTRICAL DIGITAL DATA PROCESSING
- G06F2217/00—Indexing scheme relating to computer aided design [CAD]
- G06F2217/16—Numerical modeling
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V11/00—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS prospecting or detecting by methods combining techniques covered by two or more of main groups G01V1/00 - G01V9/00
-
- G—PHYSICS
- G06—COMPUTING; CALCULATING; COUNTING
- G06F—ELECTRICAL DIGITAL DATA PROCESSING
- G06F2217/00—Indexing scheme relating to computer aided design [CAD]
- G06F2217/46—Fuselage
-
- G—PHYSICS
- G06—COMPUTING; CALCULATING; COUNTING
- G06F—ELECTRICAL DIGITAL DATA PROCESSING
- G06F3/00—Input arrangements for transferring data to be processed into a form capable of being handled by the computer; Output arrangements for transferring data from processing unit to output unit, e.g. interface arrangements
- G06F3/01—Input arrangements or combined input and output arrangements for interaction between user and computer
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V7/00—Measuring gravitational fields or waves; Gravimetric prospecting or detecting
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V3/00—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V5/00—Prospecting or detecting by the use of nuclear radiation, e.g. of natural or induced radioactivity
Similar Documents
Publication | Publication Date | Title |
---|---|---|
Pelties et al. | Three‐dimensional dynamic rupture simulation with a high‐order discontinuous Galerkin method on unstructured tetrahedral meshes | |
de la Puente et al. | Dynamic rupture modeling on unstructured meshes using a discontinuous Galerkin method | |
Zhang et al. | Traction image method for irregular free surface boundaries in finite difference seismic wave simulation | |
Martin et al. | An unsplit convolutional perfectly matched layer improved at grazing incidence for seismic wave propagation in poroelastic media | |
Tago et al. | A 3D hp‐adaptive discontinuous Galerkin method for modeling earthquake dynamics | |
Aagaard et al. | A domain decomposition approach to implementing fault slip in finite‐element models of quasi‐static and dynamic crustal deformation | |
Peter et al. | Forward and adjoint simulations of seismic wave propagation on fully unstructured hexahedral meshes | |
De Basabe et al. | Elastic wave propagation in fractured media using the discontinuous Galerkin method | |
Quintal et al. | Quasi‐static finite element modeling of seismic attenuation and dispersion due to wave‐induced fluid flow in poroelastic media | |
Di Bartolo et al. | A new family of finite-difference schemes to solve the heterogeneous acoustic wave equation | |
Liu et al. | A comparative study of finite element and spectral element methods in seismic wavefield modeling | |
Dupuy et al. | Wave propagation in heterogeneous porous media formulated in the frequency-space domain using a discontinuous Galerkin method | |
Weng et al. | Constraining frictional properties on fault by dynamic rupture simulations and near‐field observations | |
Wang et al. | Massively parallel structured multifrontal solver for time-harmonic elastic waves in 3-D anisotropic media | |
Zhang et al. | Heterogeneous distribution of the dynamic source parameters of the 1999 Chi‐Chi, Taiwan, earthquake | |
Ren et al. | Gravity gradient tensor of arbitrary 3D polyhedral bodies with up to third-order polynomial horizontal and vertical mass contrasts | |
Ye et al. | A discontinuous Galerkin method with a modified penalty flux for the propagation and scattering of acousto-elastic waves | |
Ma | A physical model for widespread near‐surface and fault zone damage induced by earthquakes | |
Causse et al. | Are stress drop and rupture velocity of earthquakes independent? Insight from observed ground motion variability | |
Barall | A grid-doubling finite-element technique for calculating dynamic three-dimensional spontaneous rupture on an earthquake fault | |
Abdelmeguid et al. | A novel hybrid finite element‐spectral boundary integral scheme for modeling earthquake cycles: Application to rate and state faults with low‐velocity zones | |
Tromp et al. | Effects of induced stress on seismic forward modelling and inversion | |
Zhang et al. | Elastic wave modelling in 3-D fractured media: an explicit approach | |
Erickson et al. | Bimaterial effects in an earthquake cycle model using rate‐and‐state friction | |
Twardzik et al. | Inversion for the physical parameters that control the source dynamics of the 2004 Parkfield earthquake |