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Gas measurements from IODP Hole 318-U1359D
Geocode = Top depth CSF-A (m) -
Gas measurements from IODP Hole 318-U1357A
Geocode = Top depth CSF-A (m) -
(Table 1) C1 - C8 volatile compounds in sediments from DSDP Leg 63 Holes
Low-temperature diagenetic reactions (less than 50°C) are held responsible for the generation of small amounts of C1-C8 hydrocarbons (less than 100 ng hydrocarbon/g dry weight... -
(Table 2) Chemical composition of gases in basalts from DSDP Leg 65 Holes
Basalts from different structural provinces in the ocean basins, such as mid-ocean ridges, island arcs, and oceanic plateaus, show marked differences in major and minor element... -
(Table 1) Low molecular weight hydrocarbon concentrations and organic carbon ...
C2-C8 hydrocarbons (36 compounds identified) from 56 shipboard sealed, deep-frozen core samples of DSDP Leg 71, Site 511, Falkland Plateau, South Atlantic, were analyzed by a... -
(Table 1) Summary of low-molecular-weight hydrocarbon concentrations, organic...
A series of core samples taken during Cruise 79 of Glomar Challenger, drilling offshore Morocco (Mazagan Plateau), is analyzed for their low-molecular-weight hydrocarbon... -
(Table 1) Organic carbon, hydrogen and oxygen index and hydrocarbons at DSDP ...
C2-C8 hydrocarbon concentrations (about 35 compounds identified, including saturated, aromatic, and olefinic compounds) from 27 shipboard-sealed, deep-frozen core samples of... -
Gas measurements from IODP Hole 317-U1354C
Geocode = Top depth CSF-A (m).Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30:... -
Gas measurements from IODP Hole 317-U1353B
Geocode = Top depth CSF-A (m).Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30:... -
Gas measurements from IODP Hole 317-U1352C
Geocode = Top depth CSF-A (m).Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30:... -
Gas measurements from IODP Hole 317-U1352B
Geocode = Top depth CSF-A (m). Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30:... -
Gas measurements from IODP Hole 317-U1352A
Geocode = Top depth CSF-A (m).Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30:... -
Gas measurements from IODP Hole 317-U1351B
Geocode = Top depth CSF-A (m). Introduction to shipboard organic geochemistry on the JOIDES Resolution; ODP Technical Note 30:... -
Analyses of gashydrates from DSDP Sites 76-533 and 84-568 (Table 1)
Two sites of the Deep Sea Drilling Project in contrasting geologic settings provide a basis for comparison of the geochemical conditions associated with marine gas hydrates in... -
(Table 1b) Relative composition of light hydrocarbons of collection site GeoB...
Relative composition of light hydrocarbons (in mol% Σ(C1−C6)] and resulting C1/(C2−C6) ratios in gas (Chapopote) and oil (Mictlan) bubbles above invertebrate collection sites. -
(Table 1a) Concentrations of low-molecular-weight alkanes in gas samples of c...
Concentrations of low-molecular-weight alkanes [in mmol L-1 bulk asphalt] and resulting C1/(C2–C5) ratios in gas samples prepared from an asphalt/gas hydrate piece from one of... -
Concentrations of dissolved anions in porewater and gaseous alkanes in sedime...
The Guaymas Basin hydrothermal vents in the Gulf of California (Mexico) were visited with the research vessel RV Atlantis in November to December 2018 (mission AT 42-05). Due to... -
Exploring the Catalytic Pathway of Butane Isomerisation
The petrochemical industry accounts for a large proportion of global chemical industry, as such even subtle improvements in product yield can result in significant economic and... -
(Table 1) Hydrocarbon gas composition of sediment and gas hydrate collected i...
In the Campeche Knolls, in the southern Gulf of Mexico, lava-like flows of solidified asphalt cover more than 1 square kilometer of the rim of a dissected salt dome at a depth... -
Gas composition in sedimentary rocks from Heiss-1 Hole drilled in the Heiss I...
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