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Strength and deformation behavior of ODP Leg 110 sediments
The shape and morphology of the northern Barbados Ridge complex is largely controlled by the sediment yield and failure behavior in response to high lateral loads imposed by... -
Magnetic susceptibility anisotropy in deformed sediments of ODP Leg 110
The anisotropy of magnetic susceptibility documents the generation of tectonically produced fabrics in sediments that macroscopically show no evidence of this disruption. The... -
Bulk chemical analysis of sediments ODP Hole 110-671B and 110-672A
Chemical analyses for calcium carbonate, organic carbon, and major constituents (Al, Ti, Ca, Mg, K, Fe) of bulk sediments collected in Hole 671B have been carried out. Organic... -
Bulk and clay mineralogy of ODP Leg 110 holes
The mineralogy of both bulk- and clay-sized fractions of samples from Sites 671, 672, and 674 of ODP Leg 110 was determined by X-ray diffraction. The major minerals include... -
Oxygen isotope composition of clinoptilolites
Oxygen isotope ratios were obtained from authigenic clinoptilolites from Barbados Accretionary Complex, Yamato Basin, and Exmouth Plateau sediments (ODP Sites 672, 797, and 762)... -
Stable isotope ratios of interstitial fluids from ODP Leg 110 sites
Delta18O values of pore waters from the northern Barbados accretionary prism range from -0.3 to -3.6 per mil and reflect pervasive reaction of volcanic ash to form smectite... -
(Table 4) Strontium isotope ratios of ODP Leg 110 samples
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(Table 3) Br/Cl and NH4 concentrations of interstitial water of ODP Leg 110 s...
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(Table 2) Geochemistry of interstitial water of ODP Leg 110 samples
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(Table 1) Geochemistry of interstitial waters from different experiments from...
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Interstitial water chemistry of ODP Leg 110 holes
Major-element compositions (Cl-, SO4[2-], Ca2+, Mg2+ , Li+ , K+, Na+ , Sr2+) of interstitial waters obtained from sediment cores along the ODP Leg 110 transect across the...