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(Table 2) Experimental testing and best-fit curve measurements on unsheared s...
This dataset has no description
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(Table T4) Hydraulic conductivities and gradients of sediments from ODP Leg 2...
This dataset has no description
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(Table T6) Consolidation properties and permeabilities of sediments from ODP ...
This dataset has no description
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(Table 3) Calculated consolidation times for sedimentary sections of the Pryd...
For T = 0.05 (and less), only the top of the sediment, immediately beneath the applied load, is consolidated, whereas for T = 1, the sedimentary section is fully consolidated... -
(Table 2) Triaxial stress conditions ans shear strength parameters of ODP Leg...
This dataset has no description
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(Appendix 1) Temperature, ionic strength, and porewater activity from ODP Leg...
Depth, sediment is given in mbsf. See also Inoue (2000b) dataset: doi:10.1594/PANGAEA.788861. -
(Table 16) Bitumen characteristics of organic matter in Black Sea sediments f...
This dataset has no description
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(Table 2) Fission track ages of apatite and sphene from Paleogene sediments a...
Fission track ages of individual crystals of detrital apatite and sphene separated from early Eocene and Paleocene sandstones at Site 555 indicate the contribution of detritus... -
(Table 1) Summary of one-dimensional consolidation test results for ODP Leg 1...
Most of the sediments at Sites 819 through 821 are underconsolidated, likely the result of high sedimentation rates. Normally consolidated sediments appear at intervals of low... -
Geotechnical and physical properties from whole-round consolidations samples ...
Sediments cored from the Barbados Ridge accretionary complex at ODP Sites 671, 672, and 676 are progressively underconsolidated with depth. Very low measured intergranular... -
(Table 1) U-Pb isotopic results of single-grain zircon and monazite analyses,...
At Elan Bank of the Kerguelen Plateau in the southeast Indian Ocean, Leg 183 of the Ocean Drilling Program recovered clasts of garnet-biotite gneiss in a fluvial conglomerate... -
(Table 1) Chemical compositions of beryllium in sediments and pore waters of ...
Studies of Be distributions in subduction zone sediments will help to understand questions regarding the enrichments of cosmogenic Be-10 in arc volcanic rocks. Analyses of Be-10... -
(Table 1) Geochemistry of carbonate veins from basalts of the eastern flank o...
Leg 168 of the Ocean Drilling Program (ODP) investigated the heat flow, fluid chemistry and crustal alteration associated with ridge flank hydrothermal systems. Ten sites were... -
(Table 1) Beluga (Delphinapterus leucas) density and abundance, and pod chara...
An aerial survey was conducted to estimate the abundance of belugas (Delphinapterus leucas) on their wintering ground in West Greenland in March-April 2006 and 2008. The survey... -
(Appendix A) Cd/Ca ratios of benthic foraminifera from surface deep-sea sedim...
This dataset has no description
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(Table 3) Fission track age data for zircons from ignimbrites in Taupo Volcan...
Age is fission track age, calculated using the zeta calibration method. Ignimbrites in Taupo Volcanic Zone (position is a mean of the Taupo Volcanic complex) are possible... -
(Table 2) Fission track age data for zircons from tephras
Age is fission track age, calculated using the zeta calibration method. Positions are estimated from map -
(Table 1) Fission track age data for zircons from Fish Canyon Tuff standard
Age is fission track age, calculated using the zeta calibration method -
(Appendix A) Sr/Ca ratios of benthic foraminifera from surface deep-sea sedim...
Med = Mediterranean Sea, RC = equatorial Pacific samples -
(Table 4) Iron speciation in samples from the Winter Ice Edge taken during th...
Detection window employed in this work: 10 µM TAC.
