-
(Table 2) Elastic constants and shear wave velocities of DSDP Sample 60-458-3...
This dataset has no description
-
(Table 1) Bulk densities and compressional wave velocities at DSDP Holes 60-4...
Empty cells = no data. -
(Table 2) Elastic constants and shear-wave velocities at DSDP Hole 62-465A
This dataset has no description
-
(Table 1) Compressional-wave velocities at DSDP Hole 62-465A
This dataset has no description
-
(Table 3) Anisotropy velocity (Pc = 0.2 kbar) at DSDP Holes 62-463 and 62-465A
This dataset has no description
-
(Table 1) Summary of acoustic properties at DSDP Holes 62-463 and 62-465A
Sediment depth is given in mbsf. Empty cells = no data. -
(Table 1) Velocities, densities, porosities, and elastic constants of DSDP Le...
This dataset has no description
-
(Table T1) Physical properties, and compressional and shear wave velocities a...
This dataset has no description
-
(Appendix A) Compressional and shear wave velocities, density and porosity as...
Sediment depth is given in mbsf. Q = quality factor. Attenuation = 1000/Q. -
(Table T2) Compressional and shear wave velocities of three-axis minicores fr...
This dataset has no description
-
(Table 1) Summary of acoustic properties at DSDP Leg 59 Holes
Pyroclastic and other sediments derived from volcanic terranes are prominent constituents of the sediment column in the central and eastern parts of the Philippine Sea. On the... -
(Table 1) Summary of acoustic properties at DSDP Holes 60-453 and 60-459B
Laboratory measurements of physical properties are important because the results may be applied to the interpretation of seismic and other types of geophysical data, and because... -
(Table 1) Summary of densities and compressional-wave velocities at DSDP Hole...
Compressional-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... -
(Table 1) Physical properties of sediments at DSDP Holes 79-545 and 79-547A
Laboratory measurements of the acoustic and physical properties of deep-sea sediments and rocks are important for the interpretation of seismic reflection and refraction data... -
(Table 1) Compressional and shear wave velocities and elastic constants of DS...
Compressional and shear wave velocities at confining pressures to 6 kb, densities, and porosities were measured for 32 samples obtained from 836 to 1350 m below seafloor (BSF)... -
Sensing SO2 in Robust Porous MOF Materials via Simultaneous Microwave Dielect...
We seek to develop new MOFs for sensing and removal of toxic gases (e.g., SO2) and request 4 days on POLARIS to study the structural binding details and dielectric data... -
Decomposition studies of Li(1-x)NaxND2, LiNa2(ND2)3 and Li3Na(ND2)4
We ask for 3 days on GEM to study in-situ the decomposition of the Na-substituted LiNH2 phases, Li1-xNaxND2, LiNa2(ND2)3, Li3Na(ND2)4 and their reactions with LiD. LiNH2 is the... -
IN-SITU NEUTRON DIFFRACTION STUDIES OF METAL-HYDRIDE HYDROGEN STORAGE MATERIALS
Recently [RB 900007], we have demonstrated that it is possible to determine the detailed site-by-site behaviour of hydrogen during in-situ absorption and desorption in metal...
