-
Computed tomography (CT) scanning of clasts from IODP Site 318-U1361
This dataset has no description
-
Computed tomography (CT) scanning of clasts from ODP Site 188-1165
This dataset has no description
-
Interpolated grain size analysis from IODP Site 318-U1361
This dataset has no description
-
Interpolated grain size analysis from sediment core RS15-LC42
This dataset has no description
-
(Table 2) CT scan measurements of ODP Site 131-808
X-ray computed tomography (CT) is a promising tool that yields data useful for understanding the fine-scale density structure of partly lithified and tectonically deformed... -
X-ray Computed Tomography greyscale data from IODP Hole 318-U1357B
This dataset has no description
-
Multiple proxies for sediment core P1-93AR-P23 collected from the Northwind R...
This dataset has no description
-
Multiple proxies for sediment core HLY0503-03JPC collected from the Northwind...
This dataset has no description
-
Number of gravel in Lake Lauvitel sediments
This dataset has no description
-
(Table T2) Wet and dry resistivity along three orthogonal directions of ODP H...
Sediment depth is given in mbsf. Lithology and lithologic units are as defined during Leg 185 (Shipboard Scientific Party, 2000, doi:10.2973/odp.proc.ir.185.104.2000). -
(Table T1) Wet and dry resistivity along three orthogonal directions of ODP H...
Sediment depth is given in mbsf. Resistivity values of >9999 = above detection limit of 9999.9 Ohm m. -
(Table 1) Summary of CT values, attenuation coefficients, density, and porosi...
This paper presents results of an interdisciplinary investigation of the relation between fluids, fluid flow, and deformation in the toe region of the Nankai accretionary prism.... -
(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...
