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Stable isotope ratios opf ODP Site 111-677
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(Table 1) Composition of sediment pore waters from ODP sites 111-677 and 111-678
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(Table 1) Range chart for planktonic foraminifers from ODP Hole 111-667A
species abundance: A = abundant >20 %), C = common (10-20 %), R = rare, (5-10 %) VR = very rare (<5 %), - = not observed -
(Table 1) Lithium concentration and isotopic composition of rocks from DSDP/O...
Further d18O data see Alt et al. (1986) datasets: doi:10.1594/PANGAEA.713298 and Alt et al., (1989) datasets: doi:10.1594/PANGAEA.713302 -
(Table 3) Stable oxygen and carbon isotope ratios of benthic foraminifera in ...
Depth from barrel sheets (mbsf, Shipboard Scientific Pary, 1988). Mass spectrometer VG Isogas 903 triple-collector, after October 1988 (samples A 88/2048 onward) VG Isogas SIRA... -
(Data Set S1) Compiled benthic foraminiferal stable isotopic values
d13C_adj: carbon isotopic value adjusted to Cibicidoides equivalent.d18O_adj: oxygen isotopic value adjusted to Cibicidoides equivalent. -
Hole/Core summary of ODP Site 111-678
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Hole/Core summary of ODP Site 111-677
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Hole/Core summary of ODP Site 111-504
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Results of rock eval carbon analysis on ODP Hole 111-677A
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Core/Section summary of ODP Hole 111-678B
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Pore-water chemistry of ODP sites 111-677 and 111-678
Sites 677 and 678 were drilled on ODP Leg 111 to test hypotheses about the nature and pattern of hydrothermal circulation on a mid-ocean ridge flank. Together with earlier... -
Seismic properties of sheeted dikes from ODP Hole 111-504B
Seismic velocities have been measured at confining pressures to 600 MPa for eight samples of sheeted dike rock obtained from Hole 504B during Leg ODP 111. The compressional- and... -
Lithium concentrations and isotope composition of basalt samples from ODP/DSD...
Ocean Drilling Program (ODP) Hole 504B near the Costa Rica Rift is the deepest hole drilled in the ocean crust, penetrating a volcanic section, a transition zone and a sheeted... -
Strontium chemistry of anhydrite from DSDP/ODP Hole 504B
A unique record of the chemical evolution of seawater during hydrothermal recharge into oceanic crust is preserved by anhydrite from the volcanic sequences and sheeted dike... -
X-ray fluorescence on samples of ODP Hole 111-678B
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X-ray fluorescence on samples of ODP Hole 111-677A
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X-ray fluorescence on samples of ODP Hole 111-504B
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Magnetic susceptibility on ODP Hole 111-677A
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Magnetic susceptibility on ODP Hole 111-504B
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