Figure F6. Velocity functions used to calculate reflection coefficient series for each of the three physical property processing scenarios described in text and illustrated in Figure F4. Black lines = velocity functions, blue dots = laboratory measurements of vertical (z) P-wave velocities. In Scenario 1, all measured velocities from physical properties are used to pick layers and calculate reflection coefficient series. In Scenario 2, velocities >3 km/s from thin (<1 m) lithologic intervals are removed where they were measured in Unit 5 above the upper sill (1067–1612 mbsf). In Scenario 3, the thickness spanned by high-velocity laboratory measurements is modified to represent the thickness of the corresponding lithology in core descriptions.

Figure F6. Velocity functions used to calculate reflection coefficient series for each of the three physical property processing scenarios described in text and illustrated in Figure F4. Black lines = velocity functions, blue dots = laboratory measurements of vertical (z) P-wave velocities. In Scenario 1, all measured velocities from physical properties are used to pick layers and calculate reflection coefficient series. In Scenario 2, velocities >3 km/s from thin (<1 m) lithologic intervals are removed where they were measured in Unit 5 above the upper sill (1067–1612 mbsf). In Scenario 3, the thickness spanned by high-velocity laboratory measurements is modified to represent the thickness of the corresponding lithology in core descriptions.