Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves
In Vertical Seismic Profiling tube waves are generated by compressional waves impinging on subsurface fractures or permeable zones. The amplitude of tube waves is dependent upon the formation permeability, the length of the fracture, and on the source frequency. The generation of tube waves is f...
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Format: | Technical Report |
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Massachusetts Institute of Technology. Earth Resources Laboratory
2012
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Online Access: | http://hdl.handle.net/1721.1/75049 |
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author | Beydoun, W. B. Cheng, C. H. Toksoz, M. N. |
author2 | Massachusetts Institute of Technology. Earth Resources Laboratory |
author_facet | Massachusetts Institute of Technology. Earth Resources Laboratory Beydoun, W. B. Cheng, C. H. Toksoz, M. N. |
author_sort | Beydoun, W. B. |
collection | MIT |
description | In Vertical Seismic Profiling tube waves are generated by compressional
waves impinging on subsurface fractures or permeable zones. The amplitude of
tube waves is dependent upon the formation permeability, the length of the
fracture, and on the source frequency. The generation of tube waves is
formulated theoretically and the relative effects of these parameters are
studied individually. Field examples are shown for open fractures in granite.
From tube wave amplitudes normalized to P-wave amplitudes, calculated
permeabilities are on the order of 400 millidarcys. |
first_indexed | 2024-09-23T08:02:19Z |
format | Technical Report |
id | mit-1721.1/75049 |
institution | Massachusetts Institute of Technology |
last_indexed | 2024-09-23T08:02:19Z |
publishDate | 2012 |
publisher | Massachusetts Institute of Technology. Earth Resources Laboratory |
record_format | dspace |
spelling | mit-1721.1/750492019-04-09T16:14:41Z Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves Beydoun, W. B. Cheng, C. H. Toksoz, M. N. Massachusetts Institute of Technology. Earth Resources Laboratory Beydoun, W. B. Cheng, C. H. Toksoz, M. N. In Vertical Seismic Profiling tube waves are generated by compressional waves impinging on subsurface fractures or permeable zones. The amplitude of tube waves is dependent upon the formation permeability, the length of the fracture, and on the source frequency. The generation of tube waves is formulated theoretically and the relative effects of these parameters are studied individually. Field examples are shown for open fractures in granite. From tube wave amplitudes normalized to P-wave amplitudes, calculated permeabilities are on the order of 400 millidarcys. 2012-11-27T20:28:07Z 2012-11-27T20:28:07Z 1983 Technical Report http://hdl.handle.net/1721.1/75049 Earth Resources Laboratory Industry Consortia Annual Report;1983-10 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory |
spellingShingle | Beydoun, W. B. Cheng, C. H. Toksoz, M. N. Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves |
title | Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves |
title_full | Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves |
title_fullStr | Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves |
title_full_unstemmed | Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves |
title_short | Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves |
title_sort | detection of subsurface fractures and permeable zones by the analysis of tube waves |
url | http://hdl.handle.net/1721.1/75049 |
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