(Table 5) Stable oxygen isotope ratios of pore waters from ODP Site 166-1007
| Cobertura |
MEDIAN LATITUDE: 24.504300 * MEDIAN LONGITUDE: -79.322400 * SOUTH-BOUND LATITUDE: 24.504200 * WEST-BOUND LONGITUDE: -79.322500 * NORTH-BOUND LATITUDE: 24.504400 * EAST-BOUND LONGITUDE: -79.322300 * DATE/TIME START: 1996-03-29T06:30:00 * DATE/TIME END: 1996-04-08T15:18:00 * MINIMUM DEPTH, sediment/rock: 5.95 m * MAXIMUM DEPTH, sediment/rock: 708.36 m |
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| Data(s) |
08/11/2000
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| Formato |
text/tab-separated-values, 184 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.800269 doi:10.1594/PANGAEA.800269 |
| 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 | #166-1007B; 166-1007C; delta 18O, standard deviation; delta 18O, water; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Isotope ratio mass spectrometry; Joides Resolution; Leg166; North Atlantic Ocean; Ocean Drilling Program; ODP; ODP sample designation; Sample code/label |
| Tipo |
Dataset |
