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Seismic anisotropy in gas-hydrate- and gas-bearing sediments on the Blake Ridge, from a walkaway vertical seismic profile
University of Texas, Austin, Texas, USA
University of Wyoming, Laramie, Wyoming, USA
University of Texas, Austin, Texas, USA
Georgia Institute of Technology, Atlanta, Georgia, USA
Naval Research Laboratory, Stennis Space Center, Mississippi, USA
U.S. Geological Survey, Woods Hole, Massachusetts, USA
U.S. Geological Survey, Woods Hole, Massachusetts, USA
Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
We present results from an analysis of anisotropy in marine sediments using walkaway vertical seismic profiles from the Blake Ridge, offshore South Carolina. We encountered transverse isotropy (TI) with a vertical symmetry axis in a gas-hydrate-bearing unit of clay and claystone with Thomsen parameters ε = 0.05 ± 0.02 and δ = 0.04 ± 0.06. TI increased to ε = 0.16 ± 0.04 and δ = 0.19 ± 0.12 in the underlying gas zone. Rock physics modeling suggests that the observed TI is caused by a partial alignment of clay particles rather than high-velocity gas-hydrate veins. Similarly, the increase of TI in the gas zone is not caused by thin low-velocity gas layers but rather, we speculate, by the sharp contrast between seismic properties of an anisotropic sediment frame and elongated gas-bearing pore voids. Our results underscore the significance of anisotropy for integrating near-vertical and wide-angle seismic data.
Received 13 April 2003; accepted 21 May 2003; published 17 July 2003.
Citation: (2003), Seismic anisotropy in gas-hydrate- and gas-bearing sediments on the Blake Ridge, from a walkaway vertical seismic profile, Geophys. Res. Lett., 30(14), 1733, doi:10.1029/2003GL017477.
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