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Trace elemental data from the Cretaceous–Paleogene boundary (K-Pg boundary)
Trace elemental data from the K-Pg boundary -
Total calcareous nannofossils abundance and accumulation rates over the past ...
This dataset has no description
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Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
(Table 1) Carbon and oxygen isotope ratios and depth of formation of authigen...
Carbonate concretions in Pliocene to Miocene diatomaceous sediments at Sites 438, 439, and 584 on the deep-sea terrace near the Japan Trench are composed of calcite, dolomite,... -
Correlation of Late Jurassic and Early Cretaceous zonation events in ODP and ...
A database was built of 378 stratigraphic events, including first and last stratigraphic occurrences (FO/LO) of calcareous nannofossils, foraminifers, and dinocysts, and... -
Compilation of global mid-Miocene opal distribution
This is a virtual data set that comprises several other real data sets. -
Geochemistry and geological ages for organic-rich black shales of the Quatern...
This dataset has no description
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Physical properties at DSDP Holes 77-535 and 77-540
Tables 1 and 2 contain the data for the physical properties of the material from Sites 535 and 540, respectively. These data are summarized for Site 535 in Table 23 and Figure... -
Grain-size, carbon and calcium carbonate at DSDP Leg 77 Holes
Sand-silt-clay distribution was determined on 10-cm**3 sediment samples collected at the time the cores were split and described. Supplement to: Bode, Gerald W (1984): Appendix... -
Inclination of the two main components of magnetization and 87Sr/86Sr ratios ...
Site 536 terminated in a shallow-water dolomite of unknown age. Paleomagnetic measurements combined with strontium isotope analyses suggest that the dolomite was deposited in... -
Magnetic properties and chemical composition at DSDP Hole 77-538A
Magnetic properties of doleritic and some metamorphic basement rocks underlying Catoche Knoll are studied. Doleritic rocks show a high saturation magnetic moment (2-5 emu/g)... -
Magnetic viscosity and paleomagnetism of the basement complex at DSDP Hole 77...
The basement at Catoche Knoll consists of Paleozoic gneiss and amphibolite intruded by several generations of early Jurassic diabase dikes. Upon exposure to a 1-oersted field... -
40Ar/39Ar analysis for incremental heating experiments at DSDP Holes 77-537 a...
Drilling penetrated pre-Mesozoic crystalline basement beneath abbreviated sedimentary sequences overlying fault blocks in the southeastern Gulf of Mexico. At Hole 538A, located... -
Geochemistry and petrography of organic matter at DSDP Hole 77-535
Organic geochemical and organic petrographic methods were used to study three Lower to middle Cretaceous sediment samples from Hole 535 in the southeastern Gulf of Mexico for... -
Lithology and organic geochemistry at DSDP Hole 77-535
Analyses of extractable organic matter from selected core samples obtained at DSDP Site 535 in the eastern Gulf of Mexico show that the asphalt (or tar) and adjacent oil stains... -
Organic geochemistry of lower Cretaceous sediments at DSDP Hole 77-535
At Site 535, the four lithologic units of Cretaceous age are controlled by two types of sedimentologic facies: (1) the massive light-colored limestones or marly limestones in... -
Geochemistry and pyrolysis at DSDP Hole 77-535
There are substantial differences in the character of organic matter contained in the Pleistocene and Cretaceous sedimentary sequences of DSDP Site 535. The argillaceous... -
Porosity, permeability, trace elements, and carbon-oxygen isotopes at DSDP Ho...
Talus deposits recovered from Site 536 show evidence of aragonite dissolution, secondary porosity development, and calcite cementation. Although freshwater diagenesis could... -
Investigations of Cretaceous and Tertiary kerogens in sediments of ODP Leg 11...
Seventy-one samples from nine sites were analyzed for total organic carbon (TOC). Fifty-six samples, containing 0.2% or more TOC, were evaluated by Rock-Eval to assess the... -
Abundance of planktic foraminiferal species in sediments at DSDP Sites 10-95,...
Over most of the Gulf of Mexico and Caribbean a hiatus is present between the lower upper Maastrichtian and lowermost Tertiary deposits; sedimentation resumed ~200 ka (upper...