(Table 6) Geochemistry and degree of organic carbon preservation in the laminated part of the Tard Clay, well Ad 3
| Cobertura |
LATITUDE: 47.000000 * LONGITUDE: 19.000000 * MINIMUM DEPTH, sediment/rock: 630.5 m * MAXIMUM DEPTH, sediment/rock: 677.3 m |
|---|---|
| Data(s) |
20/07/1994
|
| Formato |
text/tab-separated-values, 133 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.763274 doi:10.1594/PANGAEA.763274 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.763277 Brukner-Wein, Alice; Hetényi, Magdolna; Vetó, István (1990): Organic geochemistry of an anoxic cycle: A case history from the Oligocene section, Hungary. Organic Geochemistry, 15(2), 123-130, doi:10.1016/0146-6380(90)90077-D Vetó, István; Hetényi, Magdolna; Demény, Attila; Hertelendi, Ede (1994): Hydrogen index as reflecting intensity of suiphidic diagenesis in non-bioturbated, shaly sediments. Organic Geochemistry, 22(2), 299-310, doi:10.1016/0146-6380(94)90176-7 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #Calculated; Carbon, organic, total; Carbon, organic total/Carbon, organic, original, ratio; Carbon analyser, LECO; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Hydrogen index, mass HC per unit mass total organic carbon; Sulfur, total; Wall_Ad3 |
| Tipo |
Dataset |
