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(Table 3) Petrological parameters of sands and sandstones from DSDP and ODP h...
Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline... -
(Table 2) Survey of Pacific Ocean DSDP sites for hiatuses PH and NH 1 through...
This dataset has no description
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(Table DR1) 10Be data for sediments from DSDP Hole 56-436
10Be model ages was calulated from radioactive decay equation: N=N_o(e-t), where N_o assumed to be 1299 million a cm-3 and 10 Be decay constant, lambda, is 1.496x10**-7 -
(Table DR1) 10Be data for sediments from DSDP Hole 56-434
10Be model ages was calulated from radioactive decay equation: N=N_o(e-t), where N_o assumed to be 1299 million a cm-3 and 10 Be decay constant, lambda, is 1.496x10**-7 -
(Table 3) Projected ages of radiolarian events of DSDP Hole 56-436 in the wes...
Ages were obtained from age/depth plots based on diatom, foraminifer, calcareous nannofossil and magnetostratigraphic events -
Age model of DSDP Hole 56-436
This dataset has no description
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Annotated record of the detailed examination of Mn deposits from DSDP Leg 56 ...
The Japan Trench area was identified a favorable place for studying convergent margins during the initial deliberations of the IPOD Active Margins Panel. The Leg 56-57 DSDP... -
(Table 1) Pigments isolated from DSDP Leg 56 Holes
A relatively well documented record of intermediate and late chlorophyll diagenesis in marine sediments now exists. Intermediate diagenetic stages include conversion of chlorins... -
(Table 1) Composition of paraffin hydrocarbons at DSDP Site 56-434
Geochemical investigation of 18 samples of sediments from Site 434 involved determining the content of organic carbon, of bitumoid A (The chloroform A-chl and alcohol-benzene... -
(Table 1) Carbon and isotopic composition of organic carbon in sediments from...
We have analyzed inorganic and organic carbons and determined the isotopic composition of both sedimentary organic carbon and inorganic carbon in carbonates contained in... -
(Table 1) Fission ages of volcanic glass in ash layers at DSDP Hole 56-436
The fission-track technique was used to date nine samples of volcanic glasses from ash layers at Deep Sea Drilling Project Site 436. Age varied from 0.138 (+0.067 -0.063) m.y.... -
(Table 1) Consolidation characteristics and physical properties for DSDP Legs...
Consolidation characteristics of marine sediments have been determined for several different geologic provinces (cf. Hamilton, 1959, 1964; Keller and Bennett, 1973; Trabant,... -
(Table 1) Lithology, mineralogy, and physical properties of Cretaceous cherts...
Cretaceous chert and porcellanite recovered at Site 436, east of northern Honshu, Japan, are texturally and mineralogically similar to siliceous rocks of comparable age at Sites... -
(Table 1) Heavy minerals at DSDP Legs 56-57 Holes
Heavy-mineral assemblages in the cored sediments from DSDP Legs 56 and 57 show a distinct change of source rocks, from older sedimentary rocks during the Oligocene to volcanic... -
(Table 1) Typical trace-fossil occurrences in DSDP Holes 56-436 and 56-435A
Trace fossils are in places abundant in cores from DSDP Leg 56 sites. They are particularly rich in the pelagic-clay sequence at Site 436. Some significant trace fossils,... -
(Table 1) Occurrence of ichthyoliths at DSDP Hole 56-436
Approximately 20 meters of the section near the bottom of Hole 436 was "unfossiliferous," overlain by middle Miocene mudstone with siliceous microfossils and underlain by... -
(Table S1) Diatom species richness from the Early Pleistocene to present
The extent to which the spatial distribution of marine planktonic microbes is controlled by local environmental selection or dispersal is poorly understood. Our ability to... -
Lithic grain and mineral composition of sand and sandstones from the Japan an...
One hundred and twenty point counts of Oligocene to Recent sands and sandstones from DSDP sites in the Japan and Mariana intraoceanic forearc and backarc basins demonstrate that... -
Mean element and biogenic silica concentrations in Arctic Ocean sediments (Ta...
Quantitative determination of biogenic silica in Late Cretaceous and Paleogene deep-sea sediment cores from the central Arctic Ocean provides evidence of open-ocean polar... -
Benthic foraminifera abundance of Hole 56-436
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)