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Three dimensional seismic data from offshore of Mauritania (West Africa) reveal tiers of normal and tear faults that are approximately parallel to the strike and dip of the slope respectively. They formed as a result of multiple episodes of down-slope creep and have propagated through 60–140m of sediment. Some intersect the seabed while others are buried and formed during earlier down-slope translation...
In this paper, we address the irregular behaviour and geometry of the gas hydrate stability zone (HSZ) inferred from reflection seismic data in relation to heat-flow measurements. The study area lies in the hanging wall of the Posolsky fault in the Southern Baikal Basin (SBB). Side-scan sonar imagery already revealed an undulating antithetic active fault structure and several isolated active vent...
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