Figure F13. A portion of the SCS line around Site 1224 after seismic high-resolution processing. The five-layered basement structure of the oceanic crust is penetrated by Hole 1224F at this site, which is consistent with the logging-derived sequence units. Also shown is the hydrothermal vein connected to the seafloor by the fault at shotpoint (SP) 16040. SP 16002 is the closest point of approach to the site.

Figure F13. A portion of the SCS line around Site 1224 after seismic high-resolution processing. The five-layered basement structure of the oceanic crust is penetrated by Hole 1224F at this site, which is consistent with the logging-derived sequence units. Also shown is the hydrothermal vein connected to the seafloor by the fault at shotpoint (SP) 16040. SP 16002 is the closest point of approach to the site.