Abstract
AbstractJoint analysis of electrical resistivity and seismic velocity data is primarily used to detect the presence of gas hydrate‐filled faults and fractures. In this study, we present a novel approach to infer the occurrence of structurally controlled gas hydrate accumulations using azimuthal seismic velocity analysis. We perform this analysis using ocean‐bottom seismic data at two sites on Vestnesa Ridge, W‐Svalbard Margin. Previous geophysical studies inferred the presence of gas hydrates at shallow depths (up to ~190–195 m below the seafloor) in marine sediments of Vestnesa Ridge. We analyze azimuthal P‐wave seismic velocities in relation with steeply dipping near‐surface faults to study structural controls on gas hydrate distribution. This unique analysis documents directional changes in seismic velocities along and across faults. P‐wave velocities are elevated and reduced by ~0.06–0.08 km/s in azimuths where the raypath plane lies along the fault plane in the gas hydrate stability zone (GHSZ) and below the base of the GHSZ, respectively. The resulting velocities can be explained with the presence of gas hydrate‐ and free gas‐filled faults above and below the base of the GHSZ, respectively. Moreover, the occurrence of elevated and reduced (>0.05 km/s) seismic velocities in groups of azimuths bounded by faults suggests compartmentalization of gas hydrates and free gas by fault planes. Results from gas hydrate saturation modeling suggest that these observed changes in seismic velocities with azimuth can be due to gas hydrate saturated faults of thickness greater than 20 cm and considerably smaller than 300 cm.
Highlights
Structural and stratigraphic features play a significant role in controlling dynamic fluid flow processes occurring in the subsurface (Bjørlykke, 2015; Spencer, 2012)
We present a novel approach to infer the occurrence of structurally controlled gas hydrate accumulations using azimuthal seismic velocity analysis
This paper documents the application of shooting along circular tracks to study azimuthal seismic velocity variations
Summary
Structural and stratigraphic features play a significant role in controlling dynamic fluid flow processes occurring in the subsurface (Bjørlykke, 2015; Spencer, 2012). Low‐density fluids, like hydrocarbon gases, tend to move upward from deeper to shallower depths due to pressure differences unless some impermeable stratum or structural feature traps them. These fluid flow processes can result in seepage of hydrocarbon gases from the seafloor (King & MacLean, 1970) and can lead to shallow gas accumulations (Dondurur et al, 2011; Judd & Hovland, 1992; Vadakkepuliyambatta, 2014). Gas hydrates are stable only up to a certain depth
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