Total organic carbon, bitumen ratio, hopane and sterane parameters of ODP Sites 128-798 and 128-799
| Cobertura |
MEDIAN LATITUDE: 38.129383 * MEDIAN LONGITUDE: 134.333200 * SOUTH-BOUND LATITUDE: 37.038433 * WEST-BOUND LONGITUDE: 133.866700 * NORTH-BOUND LATITUDE: 39.220333 * EAST-BOUND LONGITUDE: 134.799700 * DATE/TIME START: 1989-08-27T00:00:00 * DATE/TIME END: 1989-10-13T00:00:00 * MINIMUM DEPTH, sediment/rock: 41.50 m * MAXIMUM DEPTH, sediment/rock: 1081.89 m |
|---|---|
| Data(s) |
20/07/1994
|
| Resumo |
Notable compositional changes of organic matter are observed below the silica transition zone in thermally immature sediments. The increase of bitumen ratio, and hopane and sterane isomerization parameters indicate an acceleration of the kinetics of the chemical reactions which transform the organic matter. This phenomenon is probably due to the numerous mineral and textural changes induced by the transformation of amorphous biogenic silica into crystalline authigenic silica. |
| Formato |
text/tab-separated-values, 185 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.763278 doi:10.1594/PANGAEA.763278 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Lichtfouse, Eric; Rullkötter, Jürgen (1994): Accelerated transformation of organic matter below the silica transition zone in immature sediments from the Japan Sea. Organic Geochemistry, 21(5), 517-523, doi:10.1016/0146-6380(94)90102-3 |
| Palavras-Chave | #128-798; 128-799; alpha beta/beta beta Hopane; beta alpha/beta beta Hopane; beta alpha alpha/alpha alpha alpha Sterane; Bitumen; C27 sterane; C28 sterane; C29 sterane; Carbon, organic, total; Carbon analyser, LECO; COMPCORE; Composite Core; DEPTH, sediment/rock; Event label; Gas chromatography - Mass spectrometry (GC-MS); Japan Sea; Joides Resolution; Leg128; Normalized; Ocean Drilling Program; ODP |
| Tipo |
Dataset |
