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(Table 2) Pore fluid pressure at DSDP Leg 84 Sites
This dataset has no description
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(Table T9) Effective stress, fluid flux, porosity and permeability of ODP Hol...
This dataset has no description
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(Table T3) Ages of the Miocene planktonic foraminifer zonal boundaries from O...
DEPTH, sediment is given in mcd. At Site 184-1148, the Zone N12/N13 boundary is undecided, and the Zone N6/N7 boundary at 367 mcd is estimated to be ~18000 ka on the local FO of... -
(Tables T4, T5) Flow rates, hydraulic conductivities and permeabilities of OD...
This dataset has no description
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(Tables T2, T3) Flow rates, hydraulic conductivities and permeabilities of OD...
This dataset has no description
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(Tables T2, T3) Magnetostratigraphic and astronomically tuned age models for ...
This dataset has no description
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(Table T4) Flow-through permeability properties of sediments from ODP Leg 205...
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(Appendix A) Sea surface temperture reconstruction for ODP Hole 117-723A
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(Table T3) Biostratigraphic events and ages in sediments of ODP Site 202-1237
Age for the present study was modelled using paleomagnetism data. -
(Table 1) Depths of polarity zones in meters composite depth at ODP Site 177-...
Sediment depth is given in mcd. -
(Appendix A) Gas hydrate anundance in samples of different lithologies of IOD...
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(Appendix A) Gas hydrate abundance in samples of different lithologies of IOD...
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(Table VI) Surface to bottom temperature gradients determined from stable oxy...
Raw isotope data from Nelsen et al. (1986), doi:10.1594/PANGAEA.683884. Vital effect adjustment is calculated from raw delta18O data: d18O(vea) = d18O(raw) + Sigma f. -
(Table 1) Age comparison between the GPTS and ODP Site 181-1123 age model for...
Today the deep western boundary current (DWBC) east of New Zealand is the most important route for deep water entering the Pacific Ocean. Large-scale changes in deep water... -
(Table 1) Sea surface temperature reconstruction for eastern equatorial Pacif...
Significant uncertainties persist in the reconstruction of past sea surface temperatures in the eastern equatorial Pacific, especially regarding the amplitude of the glacial... -
Sea surface temperature (TEX86), marine GDGTs and BIT index from ODP Hole 161...
The TEX86H temperature proxy is a relatively new proxy based on crenarchaeotal lipids and has rarely been applied together with other temperature proxies. In this study, we... -
(Supplement) Oedometer test results for samples from IODP Sites 317-U1351, 31...
This dataset has no description
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(Table 1) Petrological description and consolidation properties of ODP Site 1...
In order to determine the shear parameters of the forearc sedimentary strata drilled during Ocean Drilling Program Leg 186, West Pacific Seismic Network, Japan Trench, eight... -
(Table T1) Permeabilities and bulk properties of ODP Hole 191-1179C
One of the objectives of drilling at Site 1179 was to search for microbes or biochemical evidence of microbial activity as part of the ongoing exploration of the depth and... -
Spacing and amplitude of IR temperature anomalies and hydrate content of sedi...
Large uncertainties about the energy resource potential and role in global climate change of gas hydrates result from uncertainty about how much hydrate is contained in marine...
