Figure F3. (A) Multichannel and single-channel seismic lines (B) along and (C) across the accretionary prism in the vicinity of ODP Site 889, showing gently deformed slope-basin deposits overlying highly deformed accretionary prism sediments and the bottom-simulating reflector (BSR) that marks the limit of gas hydrate stability (from Riedel, Collett, Malone, et al., 2006). SP = shotpoint.
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