Straightforward derivation of Hubral’s wavefront curvature differential equation in inhomogeneous isotropic media

Author:

Krey Theodor1

Affiliation:

1. Prakla‐Seismos GmbH, Haarstr. 5, Postfach 4767, D-3000 Hannover, West Gemany

Abstract

“Wavefront curvatures in three‐dimensional laterally inhomogeneous media with curved interfaces” (Hubral, 1980, this issue) shows a differential equation [formula (4.1)] which describes the alteration of the wavefront curvature matrix along a raypath in the case of an isotropic velocity v which is an arbitrary function of the locus in the three‐dimensional space. Hubral derives his equation by referring to papers of Popov and Pšenčik (1976, 1978) and Hubral (1979).

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Cited by 5 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. References;Basic Wave Analysis;2020-08-24

2. References;Seismic Wave Propagation in the Earth;1985

3. Potential and Constraints of Near Vertical Reflection Seismics in Non-Sedimentary Deep Formations;Problems and Methods for Lithospheric Exploration;1984

4. Dynamic ray tracing in an anisotropic medium;Tectonophysics;1982-12

5. TIME-TO-DEPTH MIGRATION USING WAVEFRONT CURVATURE*;Geophysical Prospecting;1982-06

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