Determination of Shear Wave Velocity and Attenuation From Waveforms in Low Velocity Formations

In boreholes where formation shear velocity is lower than borehole fluid velocity neither refracted shear waves nor pseudo-Rayleigh waves can propagate. When frequency response of the sonde does not extend to low frequencies (e.g. 2 kHz) Stoneley waves are not excited efficiently. In such cases refr...

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Main Authors: Toksoz, M. Nafi, Wilkens, R. H., Cheng, C. H.
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2012
Online Access:http://hdl.handle.net/1721.1/75039
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author Toksoz, M. Nafi
Wilkens, R. H.
Cheng, C. H.
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Toksoz, M. Nafi
Wilkens, R. H.
Cheng, C. H.
author_sort Toksoz, M. Nafi
collection MIT
description In boreholes where formation shear velocity is lower than borehole fluid velocity neither refracted shear waves nor pseudo-Rayleigh waves can propagate. When frequency response of the sonde does not extend to low frequencies (e.g. 2 kHz) Stoneley waves are not excited efficiently. In such cases refracted P, leaking modes (PL) and fluid waves become dominant phases on a full waveform acoustic log. The P wave velocity can be determined from the first arrivals. Then, using synthetic microseismograms and a waveform matching technique, formation shear wave velocity and attenuation can be determined. This method· is demonstrated using data from a well in the Baltimore Canyon Trough area of the Atlantic margin.
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spelling mit-1721.1/750392019-04-12T20:28:05Z Determination of Shear Wave Velocity and Attenuation From Waveforms in Low Velocity Formations Toksoz, M. Nafi Wilkens, R. H. Cheng, C. H. Massachusetts Institute of Technology. Earth Resources Laboratory Toksoz, M. Nafi Wilkens, R. H. Cheng, C. H. In boreholes where formation shear velocity is lower than borehole fluid velocity neither refracted shear waves nor pseudo-Rayleigh waves can propagate. When frequency response of the sonde does not extend to low frequencies (e.g. 2 kHz) Stoneley waves are not excited efficiently. In such cases refracted P, leaking modes (PL) and fluid waves become dominant phases on a full waveform acoustic log. The P wave velocity can be determined from the first arrivals. Then, using synthetic microseismograms and a waveform matching technique, formation shear wave velocity and attenuation can be determined. This method· is demonstrated using data from a well in the Baltimore Canyon Trough area of the Atlantic margin. Massachusetts Institute of Technology. Full Waveform Acoustic Logging Consortium 2012-11-27T19:43:54Z 2012-11-27T19:43:54Z 1984 Technical Report http://hdl.handle.net/1721.1/75039 Earth Resources Laboratory Industry Consortia Annual Report;1984-08 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Toksoz, M. Nafi
Wilkens, R. H.
Cheng, C. H.
Determination of Shear Wave Velocity and Attenuation From Waveforms in Low Velocity Formations
title Determination of Shear Wave Velocity and Attenuation From Waveforms in Low Velocity Formations
title_full Determination of Shear Wave Velocity and Attenuation From Waveforms in Low Velocity Formations
title_fullStr Determination of Shear Wave Velocity and Attenuation From Waveforms in Low Velocity Formations
title_full_unstemmed Determination of Shear Wave Velocity and Attenuation From Waveforms in Low Velocity Formations
title_short Determination of Shear Wave Velocity and Attenuation From Waveforms in Low Velocity Formations
title_sort determination of shear wave velocity and attenuation from waveforms in low velocity formations
url http://hdl.handle.net/1721.1/75039
work_keys_str_mv AT toksozmnafi determinationofshearwavevelocityandattenuationfromwaveformsinlowvelocityformations
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AT chengch determinationofshearwavevelocityandattenuationfromwaveformsinlowvelocityformations