(Table 4) Stable oxygen isotope ratios of pore waters from ODP Hole 166-1006A
| Cobertura |
LATITUDE: 24.399800 * LONGITUDE: -79.459000 * DATE/TIME START: 1996-03-20T05:54:00 * DATE/TIME END: 1996-03-24T04:40:00 * MINIMUM DEPTH, sediment/rock: 2.93 m * MAXIMUM DEPTH, sediment/rock: 275.95 m |
|---|---|
| Data(s) |
08/11/2000
|
| Formato |
text/tab-separated-values, 134 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.800268 doi:10.1594/PANGAEA.800268 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.800270 Swart, Peter K (2000): The oxygen isotopic composition of interstitial waters: evidence for fluid flow and recrystallization in the margin of Great Bahama Bank. In: Swart, PK; Eberli, GP; Malone, MJ; Sarg, JF (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 166, 1-8, doi:10.2973/odp.proc.sr.166.130.2000 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Palavras-Chave | #166-1006A; delta 18O, standard deviation; delta 18O, water; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Isotope ratio mass spectrometry; Joides Resolution; Leg166; North Atlantic Ocean; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label |
| Tipo |
Dataset |
