(Table 1) Summary of densities and compressional-wave velocities at DSDP Hole 72-516F

10.1594/PANGAEA.811466Gebhard, S NS NGebhardCarlson, Richard LRichard LCarlson(Table 1) Summary of densities and compressional-wave velocities at DSDP Hole 72-516FPANGAEA1983Sample code/labelDensity, wet bulkDEPTH, sediment/rockVelocity, compressional waveDrilling/drill rigDSDP/ODP/IODP sample designationPulse transmission technique (Birch, 1960)Leg72Glomar ChallengerDeep Sea Drilling Project (DSDP)1980-03-11T00:00:00Supplementary Dataset10.2973/dsdp.proc.72.125.198390 data pointstext/tab-separated-valuesCreative Commons Attribution 3.0 UnportedCompressional-wave velocities were measured in 9 samples from the 18 m of igneous basement penetrated by drilling at Hole 516F. Wet-bulk densities range from 2.50 to 2.92 g/cm**3; compressional-wave velocities (measured at 0.4 kbar confining pressure) range from 4.29 to 6.32 km/s. Because of progressive alteration, compressional-wave velocities in deep-sea basalts tend to decrease with age; velocities in basalts from immediately beneath the sediment/basement contact are consistent with the proposed age (86 ± 4 Ma) of basement at the site. A very strong vertical velocity gradient of 0.126 km/s/m in the 18-m basement interval reflects a marked decrease in the degree of alteration with depth beneath the contact.Supplement to: Gebhard, S N; Carlson, Richard L (1983): Compressional-wave velocities in basalts from the Rio Grande Rise. In: Barker, PF; Carlson, RL; Johnson, DA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 72, 577-579-35.285-30.2765South Atlantic/CONT RISE