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Supplementary Table 2 - Trace elements of IODP Site 321-U1338
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Results for the anisotropy of magnetic susceptibility for IODP site 318-U1356A
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Anisotropy of magnetic susceptibility for IODP site 318-U1361A
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Anisotropy of magnetic susceptibility for IODP site 318-U1359D
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Anisotropy of magnetic susceptibility for IODP site 318-U1359C
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Anisotropy of magnetic susceptibility for IODP site 318-U1359B
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Anisotropy of magnetic susceptibility for IODP site 318-U1359A
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Anisotropy of magnetic susceptibility for IODP site 318-U1356A
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(Table S8) Re-Os analyses of sediment leaches and associated age corrections ...
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(Table 3) Correction of previously applied stress for the pore-pressure effec...
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(Tables T39,T41,T45,T47,T51,T53) Ko-consolidated undrained test results and p...
All stresses / pressures were originally measured in ksc (kgf/cm**2). The conversion of ksc to SI units is 1 ksc = 98.07 kPa. Tables T43, T49, T55 and T57 have been omitted... -
(Tables T38,T40,T44,T46,T50,T52) Ko-consolidated undrained test results and c...
All stresses / pressures were originally measured in ksc (kgf/cm**2). The conversion of ksc to SI units is 1 ksc = 98.07 kPa. Tables T42, T48, T54 and T56 have been omitted... -
(Table S3) Argon geochemistry of plagioclase from DSDP Site 55-433
The parameter J, a measure of the extent of conversion of 39K to 39Ar, was determined for each sample by analyzing co-irradiated Fish Canyon sanidine (FCs). Errors in this table... -
Pliocene benthic foraminiferal oxygen isotope ratios from IODP Site U1313
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(Table 1) Sodium concentrations and correction, normalization and charge-bala...
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(Table 2) Chemical composition of metalliferous sediments from DSDP Hole 34-319
Data have been corrected to a salt and CaCO3 free basis except for Ca. Leaching has been carried out by shaking 100 mg fractions in a 3.0 pH mixture of 0.2 M ammonium oxalate... -
(Table 3) Age determination of ODP Site 181-1119
Laboratory determinations were provided by the Australian Nuclear Science and Technology Organisation. Dates were corrected for marine reservoir age after the data provided by... -
(Table 4) Estimation of surface-water paleotemperatures of ODP Site 133-811 i...
To account for salinity variations first 0.5‰ was subtracted from the delta180 value. The result was then divided by 0.23 (after Epstein et al., 1953), and added to the... -
(Table 1) Apparent ages from 40Ar/39Ar heating steps for DSDP Hole 72-516F ba...
Submarine basalts are difficult to date accurately by the potassium-argon method. Dalrymple and Moore (1968) and Dymond (1970), for example, showed that, when the conventional... -
(Table 1) Current ripples from the trench outer slope, ODP Hole 131-808C
The Ocean Drilling Program Leg 131, which drilled in the Nankai Trough in the western Pacific Ocean, has shown for the first time that turbidity currents are deflected and...
