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(Supplement S3) Volcanic ash layer description and thickness analysis from di...
This dataset has no description
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(Table 1) Results from XRD analysis as well as sediment type and selected res...
The location of the seaward tip of a subduction thrust controls material transfer at convergent plate margins, and hence global mass balances. At approximately half of those... -
(Table 1) Rates of biological activity in deep-sea sediments
Global maps of sulfate and methane in marine sediments reveal two provinces of subsurface metabolic activity: a sulfate-rich open-ocean province, and an ocean-margin province... -
Detrital zircon U/Pb ages from the Nankai subduction zone (Japan)
U-Pb zircon age dating was applied on U-channel samples (30cc) that were collected from sandy deposits in cores from IODP Site C0024 (one sample; frontal Nankai accretionary... -
Table 4: Directly-measured friction velocity dependence
MS = Megasplay, Dec = Decollement.Japan Trench data from from Ikari et al. (2015). -
Table 3: Input parameters to model velocity-dependent friction parameters
Japan Trench data from Ikari et al. (2015). -
Table 2: Model-extracted velocity-dependent friction parameters
Japan Trench data from Ikari et al. (2015). -
(Supplement S1) Volcanic ash layer description and thickness analysis from di...
This dataset has no description
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Flow rates, hydraulic conductivities and permeabilities of sediments from ODP...
Understanding the role of fluids in active accretionary prisms requires quantitative knowledge of parameters such as permeability. We report here the results of permeability... -
n-Alkane, fatty acid and hopanoic acid concentrations of ODP Site 190-1178 sa...
Ocean Drilling Program (ODP) Leg 190 was programmed to investigate deformational, diagenetic, and hydrologic processes and their interactions in the Nankai Trough accretionary... -
Permeability, overburden stress and friction coefficients of ODP Hole 190-117...
Permeability measured on three samples in a triaxial cell under effective confining pressure from 0.2 to 2.5 MPa ranges from 10-18 to 10-19 m2. Overall, results indicate that... -
Mineral composition and experimental results from XRD analyses of sediments f...
X-ray diffraction analyses of the clay-sized fraction of sediments from the Nankai Trough and Shikoku Basin (Sites 1173, 1174, and 1177 of the Ocean Drilling Program) reveal... -
Mineral composition of sediments from ODP Leg 190 sites and DSDP Hole 31-297
This data report documents the acquisition of two new sets of normalization factors for semiquantitative X-ray diffraction analyses. One set of factors is for bulk sediment... -
Sedimentological, petrographical and biostratigraphical characteristics of OD...
Leg 190 was the first of a two-leg program across the Nankai accretionary prism and Trough, offshore Japan, aiming to evaluate existing models for prism evolution and to... -
Cation exchange capacity and water content of ODP sites from Nankai
Pore fluid chlorinity lower than seawater is often observed in accretionary wedges and one of the possible causes of pore water freshening is the smectite to illite reaction.... -
Organic geochemistry of deep sea sediments from the Nankai Trough and the Sou...
Earth's largest reactive carbon pool, marine sedimentary organic matter, becomes increasingly recalcitrant during burial, making it almost inaccessible as a substrate for... -
P-wave velocity (PWS split-core system) on ODP Hole 190-1178B
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 190-1178A
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 190-1177A
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 190-1176A
This dataset has no description
