Two SHIPS seismic reflection lines crossed the Seattle fault zone, which comprises a number of individual fault splays, line PS-1 in the west and line PS-2 in the east close to downtown Seattle (Fig 1 ...

Figure 4: Calculated reflection coefficient (C r) for R2 for P–P reflections plotted against incidence angle, and interpretation carton of the LAB. For the image in Fig. 3a we conducted a ...

used a new low-energy technique to map oceanic finestructure. In this method, seismic reflection profiles were used to determine where the warm Kuroshio current meets the cold Oyashio current in ...

Precise determination of the thickness of the continental lithosphere and the magnitude and depth range of the velocity gradient at its base has proved challenging with existing seismic techniques.

DHIs are features in seismic reflection data attributed to accumulations of oil and gas. Older strata may yield direct hydrocarbon indicators (DHIs) in environments typically thought unlikely to ...