Assessing Sinkhole Potential at Wink and Daisetta Using Gravimetry and Radar Interferometry

J. Paine; S. Buckley; E. Collins; C. Wilson; W. Kress

doi:10.3997/2214-4609-pdb.157.sageep054

Assessing Sinkhole Potential at Wink and Daisetta Using Gravimetry and Radar Interferometry
By J. Paine, S. Buckley, E. Collins, C. Wilson and W. Kress
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 22nd EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems, Mar 2009, cp-157-00059
DOI: https://doi.org/10.3997/2214-4609-pdb.157.sageep054

Abstract

Large sinkholes (50 to 200 m in diameter) formed over Permian bedded salt near Wink in western Texas in June 1980 and May 2002 and on the flank of a salt dome at Daisetta, Texas in May 2008. Residents,<br>government officials, and industry representatives would like to better understand the potential for sinkhole formation and growth.

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2009-03-29

2024-04-25

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Assessing Sinkhole Potential at Wink and Daisetta Using Gravimetry and Radar Interferometry

Abstract

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The natural combination of full and image‐based waveform inversion

Poststack diffraction imaging using reverse‐time migration

Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

Fracture detection by Gaussian beam imaging of seismic data and image spectrum analysis

Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture