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Sedimentology of piston core PS08/011
This dataset has no description
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Sedimentology of piston core PS1145-6
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(Table 1) Consolidation test for sediments of ODP Leg 130 sites
Consolidation tests were performed on 19 samples of calcareous ooze from the Ontong Java Plateau, obtained during Ocean Drilling Program Leg 130. Rebound curves from... -
(Table 3) Sediment consolidation properties at DSDP Leg 72 Holes
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(Table 1) Physical properties from IODP Holes 308-U1322B, 308-U1322D and 308-...
This dataset has no description
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(Table T5) Permeability summary of ODP Site 180-1109
Sediment depth is given in mbsf. The reported permeability for Sample 180-1109C-23X-4,43-65, was measured at 276 kPa effective stress, whereas the remainder of the samples were... -
(Table 3) Compression and stress test for ODP Site 131-808B sediments
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(Table T1) Sample characteristics and overburden stress of ODP Holes 190-1173...
This dataset has no description
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(Table 3) Consolidation characteristics and excess pore-water pressures for O...
This dataset has no description
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(Table 2) Consolidation characteristics and excess pore-water pressures for O...
This dataset has no description
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(Table 7) Consolidation stress hisory of ODP Hole 123-765B
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(Table 6) Laboratory vane shear strengths from ODP Hole 123-766A
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(Table 5) Laboratory vane shear strengths from ODP Site 123-765
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(Table 2) Consolidation test results for sediments of the Prydz Bay
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(Tables 1, 2) Geotechnical properties of sediments from the Prydz Bay
land-based laboratory analyses of the whole-round core samples -
(Table 2) Consolidation test results of ODP Leg 112 samples
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(Table 2) Geotechnical properties of Norwegian Sea sediments
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(Table 1) In situ pore pressure measurements of IODP Site 308-U1324
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(Table 1) In situ pore pressure measurements of IODP Site 308-U1322
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Measured permeability data of shales taken from Lower Silurian Longmaxi Forma...
The dataset includes the measured gas permeability data of sample L1P and L1V under different pressure conditions (confining pressure and pore pressure), in the comment you will...