Buatier, Martine D; Frueh-Green, Gretchen L; Karpoff, Anne Marie (1995): (Table 3) Oxygen and hydrogen isotope ratios, and estimation of precipitation temperature of clay fractions and authigenic quartz from ODP Site 139-858 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.667077, In supplement to: Buatier, MD et al. (1995): Mechanisms of Mg-phyllosilicate formation in a hydrothermal system at a sedimented ridge (Middle Valley, Juan de Fuca). Contributions to Mineralogy and Petrology, 122(1-2), 134-151, https://doi.org/10.1007/s004100050117
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 48.456133 * Longitude: -128.709283
Date/Time Start: 1991-08-09T00:00:00 * Date/Time End: 1991-09-09T00:00:00
Minimum DEPTH, sediment/rock: 2.79 m * Maximum DEPTH, sediment/rock: 266.17 m
Event(s):
139-858 * Latitude: 48.456133 * Longitude: -128.709283 * Date/Time Start: 1991-08-09T00:00:00 * Date/Time End: 1991-09-09T00:00:00 * Elevation: -2424.6 m * Penetration: 1279.5 m * Recovery: 230.4 m * Location: North Pacific Ocean * Campaign: Leg139 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 113 cores; 934.9 m cored; 0 m drilled; 24.6% recovery
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Sample code/label | Sample label | Buatier, Martine D | DSDP/ODP/IODP sample designation | ||
| 3 | Minerals | Minerals | Buatier, Martine D | X-ray diffraction (XRD) | ||
| 4 | Grain size description | Grain size descr | Buatier, Martine D | |||
| 5 | δ Deuterium | δD | ‰ SMOW | Buatier, Martine D | ||
| 6 | δ18O | δ18O | ‰ | Buatier, Martine D | ||
| 7 | Temperature, calculated | T cal | °C | Buatier, Martine D | Calculated | Clay-water, d18O H2O = 0 per mil. Estimates based on bond-type calculations of Savin and Lee (1988) and using mineral compositions determined by AEM analyses |
| 8 | Temperature, calculated | T cal | °C | Buatier, Martine D | Calculated | Clay-water, d18O H2O = 2.5 per mil. Estimates based on bond-type calculations of Savin and Lee (1988) and using mineral compositions determined by AEM analyses |
| 9 | Temperature, calculated | T cal | °C | Buatier, Martine D | Calculated | Quartz-water, d18O H2O = 0 per mil. Estimated from the empirical curve of Sharp and Kirschner (1994) |
| 10 | Temperature, calculated | T cal | °C | Buatier, Martine D | Calculated | Quartz-water, d18O H2O = 2.5 per mil. Estimated from the empirical curve of Sharp and Kirschner (1994) |
| 11 | Temperature, calculated | T cal | °C | Buatier, Martine D | Calculated | estimates from the calculated quartz-chlorite fractionations |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
154 data points