Seismic ray theory
V Červený, I Pšenčík - Encyclopedia of solid earth geophysics, 2020 - Springer
The ray theory belongs to the methods most frequently used in seismology and seismic
exploration for forward and inverse modelling of high-frequency seismic body waves. In …
exploration for forward and inverse modelling of high-frequency seismic body waves. In …
[图书][B] Seismic anisotropy in the Earth
V Babuska, M Cara - 1991 - books.google.com
Structural geologists are well aware of the fact that isotropic rocks are quite exceptional in
nature. Whicheverorigin, sedimentary, metamorphicormagmatic, rocks are shaped with a …
nature. Whicheverorigin, sedimentary, metamorphicormagmatic, rocks are shaped with a …
Elastic-wave velocities in anisotropic media of arbitrary symmetry—generalization of Thomsen's parameters ε, δ and γ
T Mensch, P Rasolofosaon - Geophysical Journal International, 1997 - academic.oup.com
We derive the explicit analytical expressions of the phase velocities of the three bulk waves
(qP, gS 1 and qS 2) propagating in an arbitrary direction in a homogeneous strongly …
(qP, gS 1 and qS 2) propagating in an arbitrary direction in a homogeneous strongly …
Perturbation of phase velocities in elastic orthorhombic media
A Stovas, Y Roganov, V Roganov - Geophysics, 2021 - library.seg.org
The parameterization of anisotropic models is very important when focusing on specific
signatures of seismic waves and reducing the parameter crosstalk involved in inverting …
signatures of seismic waves and reducing the parameter crosstalk involved in inverting …
Ray tracing in anisotropic media with singularities
V Vavryčuk - Geophysical Journal International, 2001 - academic.oup.com
Singularities often cause trouble in tracing rays in inhomogeneous anisotropic media. The
ray‐tracing algorithms can break down in the vicinity of the singularities because the …
ray‐tracing algorithms can break down in the vicinity of the singularities because the …
High-order perturbations of the phase velocity and polarization of qP and qS waves in anisotropic media
V Farra - Geophysical Journal International, 2001 - academic.oup.com
An approximate expression of the eikonal equation and the polarization vector may be
obtained in weakly anisotropic media from first-order perturbation theory. The advantage of …
obtained in weakly anisotropic media from first-order perturbation theory. The advantage of …
First-order ray tracing for qP waves in inhomogeneous, weakly anisotropic media
I Pšenčík, V Farra - Geophysics, 2005 - library.seg.org
We propose approximate ray-tracing equations for qP-waves propagating in smooth,
inhomogeneous, weakly anisotropic media. For their derivation, we use perturbation theory …
inhomogeneous, weakly anisotropic media. For their derivation, we use perturbation theory …
[图书][B] Inverse Problems of Wave Propagation and Diffraction: Proceedings of the Conference Held in Aix-les-Bains, France, September 23–27, 1996
G Chavent, PC Sabatier - 1997 - Springer
Program of the Conference of Aix-les-Bains (23–27 sept.1996) Page 1 Program of the
Conference of Aix-Ies-Bains (23-27 sept.1996) Sponsors: We acknowledge financial support …
Conference of Aix-Ies-Bains (23-27 sept.1996) Sponsors: We acknowledge financial support …
Sensitivity of qP-wave traveltimes and polarization vectors to heterogeneity, anisotropy and interfaces
V Farra, S Begat - Geophysical Journal International, 1995 - academic.oup.com
Using ray perturbation theory, a linear relationship is derived that describes the first-order
perturbation in slowness vectors due to elastic parameter and interface perturbations as well …
perturbation in slowness vectors due to elastic parameter and interface perturbations as well …
Elastodynamic and elastostatic Green tensors for homogeneous weak transversely isotropic media
V Vavryčuk - Geophysical Journal International, 1997 - academic.oup.com
An explicit analytical formula for the complete elastodynamic Green tensor for homogeneous
unbounded weak transversely isotropic media is presented. The formula was derived by …
unbounded weak transversely isotropic media is presented. The formula was derived by …