-
Physical properties of Hole 325-M0042A
This dataset has no description
-
Physical properties of Hole 325-M0044A
This dataset has no description
-
Physical properties of Hole 325-M0047A
This dataset has no description
-
Physical properties of Hole 325-M0048A
This dataset has no description
-
Physical properties of Hole 325-M0049A
This dataset has no description
-
Physical properties of Hole 325-M0049B
This dataset has no description
-
Physical properties of Hole 325-M0053A
This dataset has no description
-
Physical properties of Hole 325-M0054B
This dataset has no description
-
Physical properties of Hole 325-M0050A
This dataset has no description
-
Physical properties of Hole 325-M0052B
This dataset has no description
-
Physical properties of Hole 325-M0054A
This dataset has no description
-
Physical properties of Hole 325-M0052A
This dataset has no description
-
Physical properties of Hole 325-M0056A
This dataset has no description
-
Physical properties of Hole 325-M0057A
This dataset has no description
-
Physical properties of Hole 325-M0058A
This dataset has no description
-
Physical properties of Hole 325-M0035A
This dataset has no description
-
Physical properties of Hole 325-M0055A
This dataset has no description
-
(Table T1) Permeability, electrical resistivity and density of ODP Hole 193-1...
Magmatic fluids, heat fluxes, and fluid/rock interactions associated with hydrothermal systems along spreading centers and convergent margins have a significant impact on the... -
(Table T1) Density, porosity, void ratio, diffusivity and permeability of ODP...
The subduction of oceanic plates regulates crustal growth, influences arc volcanism, and refertilizes the mantle. Continental growth occurs by subduction of crustal material... -
(Table 1) Comparisons of dynamic and static Young's moduli of basalt at DSDP ...
Compressional- and shear-wave velocity logs (Vp and Vs, respectively) that were run to a sub-basement depth of 1013 m (1287.5 m sub-bottom) in Hole 504B suggest the presence of...