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(Figure F2) Orthogonal vector plots of AF demagnetization steps of IODP Hole ...
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(Fig. 8) Hysteresis parameters of IODP Hole 308-U1319A
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(Fig. 2c) Total and axial NRM of 8.26 mbsf sample from IODP Hole 308-U1319A
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(Fig. 5) SIRM/kappa ratio of IODP Hole 308-U1319A
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(Fig. 5) Kappa arm/SIRM ratio of IODP Hole 308-U1319A
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(Fig. 5c) Remanent coercive field Bcr of IODP Hole 308-U1319A
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(Fig. 5b) Greigite-sensitive rock magnetic parameter ARM dem 40mT/ARM 100mT o...
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(Fig. 5b) Greigite-sensitive rock magnetic parameter Delta GRM/Delta NRM of I...
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(Fig. 5b) Greigite-sensitive rock magnetic parameter GRM of IODP Hole 308-U1319A
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(Fig. 5a) Total organic carbon in pore water of IODP Hole 308-U1319A
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(Fig. 5a) Methane (CH4) content in pore wate of IODP Hole 308-U1319A
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(Fig. 5a) Sulfate (SO4**2-) and iron (Fe**2+) contents in pore water of IODP ...
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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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(Table 1) Physical properties of IODP Sites 308-U1322 and 308-U1324
Mud-rich mass transport deposits (MTDs) have a microfabric that is significantly different from bounding non-deformed mudstones at similar depths in the first 200 m of burial.... -
(Table 1) Magnetic susceptibility from IODP Hole 308-U1322B
The continental slope of the northern Gulf of Mexico seaward of the Mississippi Delta is characterized by very rapid Quaternary sedimentation. Thick sequences of... -
(Table 1) Boron concentration and d11B values of interstitial water from IODP...
The Integrated Ocean Drilling Program Expedition 308 (IODP308) drilled normal-pressured sediments from the Brazos-Trinity Basin IV and over-pressured sediments from the Ursa... -
(Table 2) Consolidation properties of IODP Exp308 whole rock samples
In mudstones of the Ursa Basin, Gulf of Mexico, the volume of voids to solids, or void ratio, ranges from 4 (porosity = 80%) at the seafloor to 0.6 (porosity = 37%) at 600 m...