Kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion

This work concerns with seismic pulses propagation in porous-fractured rocks. Such geological media could possess strong macroscopic spatial dispersion of seismic waves. Results of physical modelling are compared with theoretical estimations of group velocities based on linear slip model of fluid-sa...

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Main Authors: Glubokovskikh, Stanislav, Rok, V.
Format: Conference Paper
Published: European Association of Geoscientists and Engineers, EAGE 2012
Online Access:http://hdl.handle.net/20.500.11937/16999
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author Glubokovskikh, Stanislav
Rok, V.
author_facet Glubokovskikh, Stanislav
Rok, V.
author_sort Glubokovskikh, Stanislav
building Curtin Institutional Repository
collection Online Access
description This work concerns with seismic pulses propagation in porous-fractured rocks. Such geological media could possess strong macroscopic spatial dispersion of seismic waves. Results of physical modelling are compared with theoretical estimations of group velocities based on linear slip model of fluid-saturated fracture. They are in good agreement. Computer 3D full waveform simulation of compressional pulses reflection on the boundary of isotropic and transverse isotropic media with horizontal symmetry axis provide a validation that use of group velocities instead of phase ones raises accuracy of the Rueger's approximate equations when concerning utilized in practice seismic signals.
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format Conference Paper
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institution Curtin University Malaysia
institution_category Local University
last_indexed 2025-11-14T07:19:20Z
publishDate 2012
publisher European Association of Geoscientists and Engineers, EAGE
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spelling curtin-20.500.11937-169992017-09-13T15:43:55Z Kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion Glubokovskikh, Stanislav Rok, V. This work concerns with seismic pulses propagation in porous-fractured rocks. Such geological media could possess strong macroscopic spatial dispersion of seismic waves. Results of physical modelling are compared with theoretical estimations of group velocities based on linear slip model of fluid-saturated fracture. They are in good agreement. Computer 3D full waveform simulation of compressional pulses reflection on the boundary of isotropic and transverse isotropic media with horizontal symmetry axis provide a validation that use of group velocities instead of phase ones raises accuracy of the Rueger's approximate equations when concerning utilized in practice seismic signals. 2012 Conference Paper http://hdl.handle.net/20.500.11937/16999 10.3997/2214-4609.20143684 European Association of Geoscientists and Engineers, EAGE restricted
spellingShingle Glubokovskikh, Stanislav
Rok, V.
Kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion
title Kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion
title_full Kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion
title_fullStr Kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion
title_full_unstemmed Kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion
title_short Kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion
title_sort kinematic and dynamic characteristics of seismic pulses in porous-fractured rocks with effective spatial wave dispersion
url http://hdl.handle.net/20.500.11937/16999