High resolution cross-hole seismic tomography at the Backhorn test facility in Illinois, USA

Saito, Hideki; Takahashi, T.; Imayoshi, Takashi; Sakashita, Susumu

doi:10.3997/2214-4609.201410840

Cited by 1 publication

(2 citation statements)

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“…The Kankakee formation is considered as a thin high-velocity layer in the low-velocity background shale ( Figure 1). The mults of several kinds of logging measurements conducted just after drilling five boreholes indicate a good correlation between well-to-well (Saito, 1991).…”

Section: Introductionmentioning

confidence: 80%

“…Those waveforms indicate a reduction of amplitude about nine times for the waves traveling within the target zone of interest in the limestone. The lower amplitude waveform has been broadened by the presence of the lowvelocity zone which was delineated by travel-time tomography (Saito, 1991). Such lowvelocity inhomogeneity within the limestone formation appears to be a zone of low-saturation, which effect have reduced the compressional wave velocity.…”

Section: Time-frequency Analysismentioning

confidence: 98%

See 1 more Smart Citation

Analysis and evaluation of interwell seismic logging techniques for reservoir characterization. [Quarterly report], July 1--September 30, 1992

Parra¹

1992

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This report was prepared as an a w u n t of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recornmendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.

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Section: Introductionmentioning

confidence: 80%

Section: Time-frequency Analysismentioning

confidence: 98%