Swart, Peter K (2000): (Table 4) Stable oxygen isotope ratios of pore waters from ODP Hole 166-1006A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.800268, In supplement to: Swart, PK (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, https://doi.org/10.2973/odp.proc.sr.166.130.2000
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
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
Event(s):
166-1006A * Latitude: 24.399800 * Longitude: -79.459000 * Date/Time Start: 1996-03-20T05:54:00 * Date/Time End: 1996-03-24T04:40:00 * Elevation: -657.9 m * Penetration: 717.3 m * Recovery: 646.93 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 77 cores; 717.3 m cored; 0 m drilled; 90.2 % recovery
Comment:
Sediment depth is given as mbsf.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Swart, Peter K | DSDP/ODP/IODP sample designation | ||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | δ18O, water | δ18O H2O | ‰ SMOW | Swart, Peter K | Isotope ratio mass spectrometry | measurement #1 |
4 | δ18O, water | δ18O H2O | ‰ SMOW | Swart, Peter K | Isotope ratio mass spectrometry | measurement #2 |
5 | δ18O, water | δ18O H2O | ‰ SMOW | Swart, Peter K | Isotope ratio mass spectrometry | mean |
6 | δ18O, standard deviation | δ18O std dev | ± | Swart, Peter K | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
134 data points