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(Table 2) Percentage of heavy clastic minerals from different Deep-Sea Drilli...
This dataset has no description
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(Table 1) Chemical composition from different Deep-Sea Drilling Project samples
0.05 mm fraction (selected by wet sieving) was analysed because the sample volume was not sufficiently large for both chemical and mineralogical analyses. As a result of... -
(Table 19) Distribution of radiolaria in Miocene to Pleistocene sediments of ...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 53) Chemical composition of size fraction <0.001 mm from sediments of ...
This dataset has no description
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(Table 52) Chemical composition of size fraction <0.001 mm from sediments of ...
This dataset has no description
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(Table 51) Chemical composition of size fraction <0.001 mm from sediments of ...
This dataset has no description
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(Table 50) Parameter b of clay minerals and polytypes of hydromica from sedim...
This dataset has no description
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(Table 49) Mineral composition of sediments from the Japan Trench at DSDP Sit...
This dataset has no description
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(Table 48) Parameter b of clay minerals and polytypes of hydromica from sedim...
This dataset has no description
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(Table 47) Mineral composition of diatomaceous oozes from the Japan Trench at...
This dataset has no description
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(Table 46) Parameter b of clay minerals and polytypes of hydromica from sedim...
This dataset has no description
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(Table 45) Mineral composition of sediments from the Japan Trench at DSDP Sit...
Results of analyses have been abtained from V.V. Zabelin (Pacific Oceanology Institute, Far East Branch of Russian Academy of Sciences) -
(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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(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....
