1,721,125 research outputs found
Geochemistry and geological ages for organic-rich black shales of the Quaternary and Tertiary
(Table 3) Gas composition and computed temperature for two examples at DSDP Hole 64-477
(Table 3) Gas composition and computed temperature for two examples at DSDP Hole 64-47
(Table 1) Sample descriptions and geochemistry for core material at DSDP Holes 64-479 and 64-480
Laminated and nonlaminated sediments from Holes 480 and 479 have been analyzed for potential differences in the composition of organic matter. Their lipid composition is very similar and indicates a primary autochthonous microbial origin and some influx of allochthonous higher-plant detritus. The nonlaminated sections contain relatively more terrigenous plant wax detritus versus autochthonous residues and a much greater amount of perylene than the laminated sections
(Table 2) Various ratios of C1-C5 hydrocarbons at DSDP Leg 64 Hole
(Table 2) Various ratios of C1-C5 hydrocarbons at DSDP Leg 64 Hol
(Table 3) Inferred sources of lipids and kerogen of DSDP Leg 63 Holes samples based on organic geochemistry
# inidicates the dominant source of two
(Table 2) Carbon isotope composition of CH4 and CO2 at DSDP Leg 64 Holes
Empty cells and samples 64-474A-40-3, 64-477-7-1, 64-478-33-3, 64-480-21-2, 64-481A-9-5 and 64-481A-22-6 were insufficient for determination
(Table 3) Headspace chemistry of canned sediment samples from DSDP Leg 64 Holes
Empty cells are samples insufficient for determination
(Table 2) Compositional parameters for hydrocarbons and ketones in DSDP Hole 64-481A
Distance (cm) from Sill 30 m
(Table 1) Sample descriptions, carbon analyses, and analytical results for the lipids and kerogens of sediments from DSDP Leg 63 Holes
Sediment depth is given in mbsf. Empty cells mean no data
(Table 2) Approximate concentrations of some molecular markers of sediments from DSDP Leg 63 Holes
Based on dry sediment weight, empty cells mean no data
- …
