(Table 1) Stable oxygen isotope ratios of pore waters from ODP Site 166-1003
| Cobertura |
MEDIAN LATITUDE: 24.545967 * MEDIAN LONGITUDE: -79.260767 * SOUTH-BOUND LATITUDE: 24.545800 * WEST-BOUND LONGITUDE: -79.260800 * NORTH-BOUND LATITUDE: 24.546100 * EAST-BOUND LONGITUDE: -79.260700 * DATE/TIME START: 1996-02-28T13:12:00 * DATE/TIME END: 1996-03-11T09:57:00 * MINIMUM DEPTH, sediment/rock: 1.45 m * MAXIMUM DEPTH, sediment/rock: 910.14 m |
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| Data(s) |
08/11/2000
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| Formato |
text/tab-separated-values, 160 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.800265 doi:10.1594/PANGAEA.800265 |
| 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 | #166-1003A; 166-1003B; 166-1003C; 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 |
