Group velocity image of singularities for converted reflected and transmitted waves in orthorhombic anisotropic media

Abstract We define double singularity points, lines and surfaces and their group velocity images for converted reflected and transmitted PS1 and PS2 waves in layered orthorhombic media. This is performed by considering the dominant term in Taylor series for Christoffel equation defined for converted waves. We show that the group velocity image for converted wave has the same functional form as the one for pure wave modes (ellipse in 3D). The position and area of the ellipse in the group velocity domain and offset domain are also analysed. We also expand this method for two‐layer model with S1S2 wave singularity in both layers. It results in quartic (S1S1, S2S2, S1S2 and S2S1 waves) characteristic equation. In the group velocity domain, it gives two close curves: quasi‐elliptical (for pure S1S1 and S2S2 waves) and very complex curve with deflection points (for converted S1S2 and S2S1 waves).

Authors

Institutions

Publication Details

Journal
Geophysical Prospecting
Published
2025-03-17
DOI
https://doi.org/10.1111/1365-2478.70005
Citations
2
Primary Topic
Seismic Imaging and Inversion Techniques
Type
article
Field-Weighted Citation Impact
3.73

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Group velocity image of singularities for converted reflected and transmitted waves in orthorhombic anisotropic media

Alexey Stovas, Y. Roganov, V. Roganov
2 citations
Geophysical Prospecting
Seismic Imaging and Inversion Techniques
3.73
article

Group velocity image of singularities for converted reflected and transmitted waves in orthorhombic anisotropic media

Alexey Stovas, Y. Roganov, V. Roganov
article en
2 citations

Abstract

Abstract We define double singularity points, lines and surfaces and their group velocity images for converted reflected and transmitted PS1 and PS2 waves in layered orthorhombic media. This is performed by considering the dominant term in Taylor series for Christoffel equation defined for converted waves. We show that the group velocity image for converted wave has the same functional form as the one for pure wave modes (ellipse in 3D). The position and area of the ellipse in the group velocity domain and offset domain are also analysed. We also expand this method for two‐layer model with S1S2 wave singularity in both layers. It results in quartic (S1S1, S2S2, S1S2 and S2S1 waves) characteristic equation. In the group velocity domain, it gives two close curves: quasi‐elliptical (for pure S1S1 and S2S2 waves) and very complex curve with deflection points (for converted S1S2 and S2S1 waves).

Geophysical ProspectingVol. 73(5)
Norwegian University of Science and Technology (NO), Kyiv City Clinical Oncology Center (UA), V.M. Glushkov Institute of Cybernetics (UA)
National Taiwan Normal University
Openalex Percentile: Top 10%
Seismic Imaging and Inversion Techniques
3.73
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.