Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6441313 | Marine Geology | 2016 | 8 Pages |
â¢A shear zone is observed to sit immediately on a hydrate BSR.â¢The shear zone developed at the base of a partially developed failure.â¢A pre-failure gas accumulation has been interpreted.â¢The shear surface along the BSR can be critically stressed due to buoyancy.â¢A buoyancy-related model for submarine slope failure is proposed.
Interpretation of a three-dimensional (3-D) seismic dataset from offshore of Mauritania reveals a shear zone at the base of a partially developed slope failure. The shear zone is at a depth of ~Â 220Â m below the seabed, immediately above a hydrate bottom simulating reflector (BSR). We propose that a paleo-gas accumulation trapped below hydrate was the primer for what would have been a substantial submarine slope failure of ~Â 220Â m thickness, covering ~Â 50Â km2. This is based on the following observations: (a) the shear surface is, at the level of seismic resolution, coincident with some present gas accumulations located immediately below sediment that hosts hydrate; (b) there are remnants of a more extensive paleo gas accumulation that would have generated sufficient buoyancy pressure for the shear surface to be critically stressed and therefore primed the failure; (c) seismic pipes are a common seismic feature within the studied succession but absent in the area of the shear zone, which supports the hypothesis that a high gas column could have existed. This is a rare example of a shear zone that did not lead to the complete development of a slope failure. It provides the first seismic evidence that the buoyancy effect of gas below the hydrate rather than the hydrate dissociation is also a viable mechanism for large-scale slope failures.