Figure 2. Seismic lines GeodyNZ 36 and 37 (Collot et al., 1996), locations in Fig. 1, short-streamer high-resolution data collected with the R/V L’Atalante’s high-speed seismic system. TWT: two-way traveltime, CDP: common depth point. BSR strength is enhanced beneath anticlines (left) and at locations where layers crop out at the seafloor (right), both structures that are predicted to focus fluid flow. We suggest that such locations may represent gas hydrate sweet spots.