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Modelling Seismic Wave Fields

Class at Faculty of Mathematics and Physics |
NDGF003

Syllabus

* Viscoelastodynamic equations:

Linear constitutive equations for viscoelastic medium, relaxation functions. Anisotropic and isotropic viscoelastodynamic equations. Dispersion and attenuation.

* Seismic model of the medium (macro model):

Coordinate systems and metric tensors. Computer representation of the model.

* Green tensor.

* Travel times:

Kinds of travel times. Isotropic and anisotropic eikonal equations. First-arrival travel times. Ray-theory travel times, elementary waves.

* Initial-value ray tracing:

Hamiltonian ray tracing, rays as geodesics, wave-propagation metric tensor. Kinematic and dynamic ray tracing. Second and higher partial travel-time derivatives.

* Calculation of ray-theory travel times:

Two-point ray tracing, shooting methods, bending methods. Computation of travel times on regular rectangular grids. Ray cells, weighting of paraxial ray approximations. Wavefront tracing.

* Calculation of first-arrival travel times:

Network shortest-path ray tracing, grid travel-time tracing.

* Ray-theory synthetic seismograms:

Isotropic and anisotropic ray theories. Weak anisotropy. Complex-valued rays and travel times. Space-time ray theory. Gaussian beams and packets, Chapman-Maslov asymptotic theory.

* Accuracy and validity conditions of asymptotic ray methods:

Kirchhoff integrals, Fresnel zones, representation theorems, Fresnel volumes.

* Full-wave finite differences in 3-D:

Accuracy of various finite-difference schemes, grid dispersion. Waves as structural interfaces. Fast calculation of the first-arrival waveforms.

* Ray method for surface waves in Cartesian and curvilinear coordinates.

Annotation

Viscoelastodynamic equations. seismic model of the medium. Green tensor. Travel times.

Initial value ray-tracing. Calculation of ray-theory travel times. Calculation of first-arrival travel times. Ray-theory synthetic seismograms. Accuracy and validity conditions of asymptotic ray methods. Full-wave finite differences in 3-D. Ray method for surface waves in Cartesian and curvilinear coordinates.