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(Table 1) Viscosity coefficients at various temperatures of samples from ODP ...
Ocean Drilling Program (ODP) Hole 735B was drilled to a depth of 1.5 km in a tectonic window of gabbroic lower oceanic crust created at the Southwest Indian Ridge. The gabbros... -
Concentrations of organic carbon and organic matter isotopic compositions of ...
Multiple layers of sapropels occur widely in the sedimentary record of the Mediterranean Sea and record repetitions of paleoclimatic conditions that favored increased production... -
Heat flow ratios of stations from the Iberian abyssal plain (Table 1)
New heat flow observations have been made in the Iberia abyssal plain off the Galicia margin along the transeat of Ocean Drilling Program Leg 149 drill sites. in order to... -
B- and O-isotope and Mg/Ca ratios of planktonic foraminifera and estimates of...
The dominant period of Pleistocene glacial cycles changed during the mid-Pleistocene from 40,000 years to 100,000 years, for as yet unknown reasons. Here we present a... -
Organic carbon and total sulfur content and concentrations of selected molecu...
During mid-Cretaceous times large amounts of organic carbon (Corg) became sequestered in 'black shales', possibly due to 'oceanic anoxic events' characterized by the development... -
(Table 1) Oxygen and carbon isotope data of bulk carbonate and foraminiferal ...
In low and middle latitudes, the Cretaceous/Tertiary boundary is marked by a sudden and pronounced decrease in d13C values of near-surface-water carbonates and a reduction in... -
(Table 2) Mass balance calculations for ODP Hole 176-735B
Ocean Drilling Program Leg 176 deepened Hole 735B in gabbroic lower ocean crust by 1 km to 1.5 km. The section has the physical properties of seismic layer 3, and a total... -
Interval transmissivities and permeabilities in ODP Hole 129-801C (Table 2)
Bulk permeability was determined from drillstring packer measurements in ODP Hole 801C in Jurassic oceanic crust in the western Pacific. The values average 8 * 10-14 m2 over 93... -
Particel size distribution and microstructures of sediments from ODP Leg 205 ...
Ocean Drilling Program Legs 170 and 205 offshore Costa Rica provide structural observations which support a new model for the geometry and deformation response to the seismic... -
(Table 3) Age model of ODP Hole 195-1202D
This dataset has no description
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(Table 2) AMS Carbon-14 dating results for ODP Hole 195-1202B
This dataset has no description
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(Table 1) Correlation tie-points of ODP Hole 195-1202D
see doi:10.1594/PANGAEA.714366 for ODP Hole 195-1202B -
(Table 1) Correlation tie-points of ODP Hole 195-1202B
see doi:10.1594/PANGAEA.714367 for ODP Hole 195-1202D -
(Table DR1) Argon isotope data and dating for individual >63 µm amphibole gra...
Variations of global and regional silicate weathering rates and paleo-ocean circulation patterns are estimated by using radiogenic isotope records, but the effects of changes in... -
Delta 66Zn ratios and age of carbonates from ODP Site 138-849 (Table 1)
The carbonate fraction of sediment core ODP 849, leg 138, located in the eastern equatorial Pacific, mostly consisting of coccoliths, was separated and analyzed for its Zn... -
Apatite fission track analytical data for samples from ODP Leg 152
We test a new approach to understanding the tectonic evolution of passive margins by using fission-track analysis on detrital apatites from sediments deposited offshore East... -
(Table 1) 87Sr/86Sr results for the Cretaceous-Tertiary boundary, ODP Hole 17...
Previous studies of 87Sr/86Sr patterns across the Cretaceous-Tertiary (K-T) boundary have generated inconsistent results. Analyses of samples from Ocean Drilling Program Hole... -
(Table 1) H2O and CO2 contents in submarine basaltic glasses from Ontong Java...
The Ontong Java Plateau in the western Pacific is anomalous compared to other oceanic large igneous provinces in that it appears to have never formed a large subaerial plateau.... -
(Table 2) Silicon isotope data for sponge spicules from ODP Hole 113-689B
The silicon isotope composition (d30Si) of biogenic opal provides a view of the silica cycle at times in the past. Reconstructions require the knowledge of silicon isotope... -
(Table 1) First and last occurrences of the menardellid clade in sediments of...
Biostratigraphic and isotopic studies of planktic foraminifera suggest that early to middle Pliocene closure of the Central American Seaway caused vicariant speciation among...
