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(Table T64) Chemical composition of trachy-andesites from Hole 465A, Leg 62 (...
This dataset has no description
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(Table 3) Rubidium and strontium concentrations and isotope ratios of DSDP ho...
This dataset has no description
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(Table DR2) Nd-Pb-Sr isotope ratios and isotope-dilution concentrations, DSDP...
This dataset has no description
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(Table DR3) Foraminiferal oxygen and carbon isotope data for DSDP Site 62-463
Benthic foraminifera include species of Nuttalides and Gavelinella. All other species listed are planktic foraminifera. All other species listed are planktic foraminifera.... -
Strontium isotope data from DSDP Site 62-463
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(Table 2) Total number of benthic foraminifera below the K/T boundary in DSDP...
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(Table 3, part d) Trace element contents in chert and associated host sedimen...
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(Table 1, part d) Major element contents in chert and associated host sedimen...
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(Table 2) Estimated ages and plankronic foraminiferal biostratigraphy of the ...
This dataset has no description
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(Table A1) Stable isotope ratios and paleotemperature calculation of selected...
Paleotemperature estimates were calculated using the equation of Erez and Luz (1983), with seawater delta18O = -1.2 per mil PDB corresponding to a continental ice-free world... -
(Tab. 15) Distribution of benthic foraminifera in Lower Cretaceous sediments ...
A = abundant, C = common, R = rare, - = absent. Samples 62-463-71-3,53-55, 62-463-79-1,34-35 radiolarians, samples 62-463-59-2, 62-463-59-CC, 62-463-70-1,41-42,... -
(Table 2) Geochemistry and acculumation rates of DSDP Hole 62-463
Age based on nannofossil biostratigraphy by Worsley for this study, documented in Chaboudy (1984) -
(Table 1) Compressional-wave velocities and anisotropies and wet-bulk densiti...
Anisotropy in compressional-wave velocities in sedimentary rocks recovered by DSDP has been recognized by several investigators (Boyce, 1976; Tucholke et al., 1976; Carlson and... -
(Table 1) Stable-isotopes of mineral separates and whole-rock powders from al...
Hess Rise, in the western Pacific Ocean, formed in the mid-Cretaceous south of the equator and moved north with the Pacific Plate (Lancelot and Larson, 1975; Lancelot, 1978;... -
(Table 1) Geochemistry of feldspars at DSDP Holes 62-464 and 62-465A
Labradorite is the principal feldspar in tholeiitic basalt from Deep Sea Drilling Project Site 464, on northern Hess Rise. Andesine and oligoclase constitute most primary... -
(Table 2) Geochemistry at DSDP Holes 62-464 and 62-465A
Igneous rocks were recovered from three sites on Hess Rise during Deep Sea Drilling Project Leg 62: altered basalt at Site 464, at the northern end of Hess Rise; and altered... -
(Table 2) Chemistry of the organic matter at DSDP Leg 62 Holes
The wide distribution of sapropelic deposits in the sedimentary cover of the oceans, their Cretaceous age, and their possible oil- and gas-generating characteristics allow us to... -
(Table 1) Sr isotopes on carbonates at DSDP Hole 62-463
Study of 12 carbonate oozes from Deep Sea Drilling Project Hole 463, in the Mid-Pacific Mountains, suggests mean values of 0.70690 ± 0.00029 (2-sigma) and 0.70712 ± 0.00030... -
(Table 1) Mass-accumulation rates for the non-authigenic, inorganic, crystall...
Elevated regions in the central parts of ocean basins are excellent for study of accumulation of eolian material. The mass-accumulation rates of this sediment component appear...
