Figure F14. Multichannel seismic profile between Sites 1118 and 1109, with selected depths below the seafloor from Taylor, Huchon, Klaus, et al. (1999, their figure F25). The interval marked with a bold vertical bar is approximately three times thicker at Site 1118 than at Site 1109, confirming the preferential deposition of sandy turbidites along the axis of the rift. CMP = common midpoint.

Figure F14. Multichannel seismic profile between Sites 1118 and 1109, with selected depths below the seafloor from Taylor, Huchon, Klaus, et al. (1999, their figure F25). The interval marked with a bold vertical bar is approximately three times thicker at Site 1118 than at Site 1109, confirming the preferential deposition of sandy turbidites along the axis of the rift. CMP = common midpoint.