Figure F2. Topography and bathymetry (contours labeled in kilometers) in the region of the Leg 180 drilling transect, showing epicenters and focal mechanisms from Abers et al. (1997) relocated 15 km south in accord with microseismicity data (see "Shallow-Angle Moresby Normal Fault," p.16). The thin double lines locate the spreading axes (Taylor et al., 1995). G = Goodenough 1 well, N = Numbiam 1 well.

Figure F2. Topography and bathymetry (contours labeled in kilometers) in the region of the Leg 180 drilling transect, showing epicenters and focal mechanisms from Abers et al. (1997) relocated 15 km south in accord with microseismicity data (see "Shallow-Angle Moresby Normal Fault"). The thin double lines locate the spreading axes (Taylor et al., 1995). G = Goodenough 1 well, N = Numbiam 1 well.