Figure 2: Rays traced through a typical velocity model for the upper oceanic crust are shown for just below the seafloor. The sources of the ray paths are near the sea surface in a 5.6km deep ocean at ranges of 2, 4, 6, and 8km. [Swift et al., 1988]

Retun to the 2003 Fall AGU Poster

THIRD PARTY BOREHOLE SEISMIC EXPERIMENTS DURING THE OCEAN DRILLING PROGRAM

Created on December 10, 2003 by Tom Bolmer