Swart, Peter K (2000): (Table 2) Stable oxygen isotope ratios of pore waters from ODP Hole 166-1004A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.800266, 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: 24.554700 * Longitude: -79.249200
Date/Time Start: 1996-03-11T09:57:00 * Date/Time End: 1996-03-12T13:20:00
Minimum DEPTH, sediment/rock: 1.45 m * Maximum DEPTH, sediment/rock: 149.79 m
Event(s):
166-1004A * Latitude: 24.554700 * Longitude: -79.249200 * Date/Time Start: 1996-03-11T09:57:00 * Date/Time End: 1996-03-12T13:20:00 * Elevation: -418.9 m * Penetration: 200 m * Recovery: 117.49 m * Location: South Atlantic Ocean * Campaign: Leg166 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 200 m cored; 0 m drilled; 58.7 % 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:
61 data points