|
Read Full Article (file size: 733243 bytes) Cited by
GEOPHYSICAL RESEARCH LETTERS,
VOL. 30, NO. 14,
1733,
doi:10.1029/2003GL017477,
2003
Seismic anisotropy in gas-hydrate- and gas-bearing sediments on the Blake Ridge, from a walkaway vertical seismic profile
Ingo A. Pecher
University of Texas, Austin, Texas, USA
W. Steven Holbrook
University of Wyoming, Laramie, Wyoming, USA
Mrinal K. Sen
University of Texas, Austin, Texas, USA
Daniel Lizarralde
Georgia Institute of Technology, Atlanta, Georgia, USA
Warren T. Wood
Naval Research Laboratory, Stennis Space Center, Mississippi, USA
Deborah R. Hutchinson
U.S. Geological Survey, Woods Hole, Massachusetts, USA
William P. Dillon
U.S. Geological Survey, Woods Hole, Massachusetts, USA
Hartley Hoskins
Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
Ralph A. Stephen
Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
Abstract
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 ɛ = 0.05 ± 0.02 and δ = 0.04 ± 0.06. TI increased to ɛ = 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.
Index Terms: 0915 Exploration Geophysics: Downhole methods; 0910 Exploration Geophysics: Data processing; 0994 Exploration Geophysics: Instruments and techniques; 3025 Marine Geology and Geophysics: Marine seismics (0935); 5102 Physical Properties of Rocks: Acoustic properties.
Read Full Article (file size: 733243 bytes) Cited by
Citation: Pecher, I. A., W. S. Holbrook, M. K. Sen, D. Lizarralde, W. T. Wood, D. R. Hutchinson, W. P. Dillon, H. Hoskins, and R. A. Stephen
(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.
Copyright 2003 by the American Geophysical Union.
|