Barrett, T J; Friedrichsen, Hans; Fleet, A J (1983): (Table 6) Oxygen and hydrogen isotopic composition of metalliferous and pelagic sediments at DSDP Leg 70 Holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.816062, In supplement to: Barrett, TJ et al. (1983): Elemental and stable isotopic composition of some metalliferous and pelagic sediments from the Galapagos Mounds area, Deep Sea Drilling Project Leg 70. In: Honnorez, J; Von Herzen, RP; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 70, 315-323, https://doi.org/10.2973/dsdp.proc.70.116.1983
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 0.591650 * Median Longitude: -86.099100 * South-bound Latitude: 0.566700 * West-bound Longitude: -86.132200 * North-bound Latitude: 0.610200 * East-bound Longitude: -86.090000
Date/Time Start: 1979-11-15T00:00:00 * Date/Time End: 1979-11-27T00:00:00
Minimum Elevation: -2711.0 m * Maximum Elevation: -2687.0 m
Event(s):
70-506 * Latitude: 0.609800 * Longitude: -86.099800 * Date/Time: 1979-11-15T00:00:00 * Elevation: -2710.0 m * Penetration: 36.7 m * Recovery: 22.7 m * Location: North Pacific/MOUND * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 7 cores; 27.9 m cored; 8.8 m drilled; 81.5 % recovery
70-506B * Latitude: 0.610200 * Longitude: -86.091300 * Date/Time: 1979-11-15T00:00:00 * Elevation: -2711.0 m * Penetration: 20.7 m * Recovery: 20.2 m * Location: North Pacific/MOUND * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 6 cores; 20.7 m cored; 0 m drilled; 97.6 % recovery
70-506C * Latitude: 0.607700 * Longitude: -86.091300 * Date/Time: 1979-11-15T00:00:00 * Elevation: -2710.0 m * Penetration: 31.3 m * Recovery: 29.7 m * Location: North Pacific/MOUND * Campaign: Leg70 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 8 cores; 31.3 m cored; 0 m drilled; 95 % recovery
Comment:
The d18O values of Samples 12, 13, 14, and 15 are for the carbonate fraction of the ooze (typically about 80%).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | Sample code/label | Sample label | Barrett, T J | DSDP/ODP/IODP sample designation | ||
| 6 | Sample ID | Sample ID | Barrett, T J | |||
| 7 | Lithology/composition/facies | Lithology | Barrett, T J | |||
| 8 | δ18O | δ18O | ‰ | Barrett, T J | Mass spectrometry | SMOW |
| 9 | δ18O, carbonate | δ18O carb | ‰ SMOW | Barrett, T J | Mass spectrometry | Carbonate fraction of the ooze |
| 10 | δ13C, carbonate | δ13C carb | ‰ PDB | Barrett, T J | Mass spectrometry | Carbonate fraction of the ooze |
| 11 | δ Deuterium | δD | ‰ SMOW | Barrett, T J | Mass spectrometry | |
| 12 | Temperature, calculated | T cal | °C | Barrett, T J | Estimated | Nontronite formation temperatures as estimated from their oxygen isotope values |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
115 data points