Elastic properties of fractured media: Dispersion, attenuation and anisotropy due to fluid flow between pores and fractures

Bibliographic Details
Main Authors: Galvin, Robert, Gurevich, Boris
Format: Book
Published: Lambert Academic Publishing 2010
Online Access:http://hdl.handle.net/20.500.11937/38345
_version_ 1848755295510069248
author Galvin, Robert
Gurevich, Boris
author_facet Galvin, Robert
Gurevich, Boris
author_sort Galvin, Robert
building Curtin Institutional Repository
collection Online Access
first_indexed 2025-11-14T08:54:02Z
format Book
id curtin-20.500.11937-38345
institution Curtin University Malaysia
institution_category Local University
last_indexed 2025-11-14T08:54:02Z
publishDate 2010
publisher Lambert Academic Publishing
recordtype eprints
repository_type Digital Repository
spelling curtin-20.500.11937-383452017-01-30T14:19:15Z Elastic properties of fractured media: Dispersion, attenuation and anisotropy due to fluid flow between pores and fractures Galvin, Robert Gurevich, Boris 2010 Book http://hdl.handle.net/20.500.11937/38345 Lambert Academic Publishing restricted
spellingShingle Galvin, Robert
Gurevich, Boris
Elastic properties of fractured media: Dispersion, attenuation and anisotropy due to fluid flow between pores and fractures
title Elastic properties of fractured media: Dispersion, attenuation and anisotropy due to fluid flow between pores and fractures
title_full Elastic properties of fractured media: Dispersion, attenuation and anisotropy due to fluid flow between pores and fractures
title_fullStr Elastic properties of fractured media: Dispersion, attenuation and anisotropy due to fluid flow between pores and fractures
title_full_unstemmed Elastic properties of fractured media: Dispersion, attenuation and anisotropy due to fluid flow between pores and fractures
title_short Elastic properties of fractured media: Dispersion, attenuation and anisotropy due to fluid flow between pores and fractures
title_sort elastic properties of fractured media: dispersion, attenuation and anisotropy due to fluid flow between pores and fractures
url http://hdl.handle.net/20.500.11937/38345