Barnes, Jaime D; Sharp, Zachary D (2006): (Table 2) Contents of chloride components in serpentinized ultramafic rocks from DSDP Site 558 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.704721, In supplement to: Barnes, JD; Sharp, ZD (2006): A chlorine isotope study of DSDP/ODP serpentinized ultramafic rocks: Insights into the serpentinization process. Chemical Geology, 228(4), 246-265, https://doi.org/10.1016/j.chemgeo.2005.10.011
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 37.770000 * Longitude: -37.343500
Date/Time Start: 1981-10-03T00:00:00 * Date/Time End: 1981-10-03T00:00:00
Minimum DEPTH, sediment/rock: 530.66 m * Maximum DEPTH, sediment/rock: 557.02 m
Event(s):
82-558 * Latitude: 37.770000 * Longitude: -37.343500 * Date/Time: 1981-10-03T00:00:00 * Elevation: -3754.0 m * Penetration: 561.5 m * Recovery: 237.8 m * Location: North Atlantic/RIDGE * Campaign: Leg82 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 43 cores; 394.5 m cored; 0 m drilled; 60.3 % 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 | Barnes, Jaime D | DSDP/ODP/IODP sample designation | ||
3 | Chloride | Cl | % | Barnes, Jaime D | Ion chromatography | water soluble |
4 | Chloride | Cl | % | Barnes, Jaime D | Ion chromatography | structually bound |
5 | Chloride | Cl | % | Barnes, Jaime D | Ion chromatography | total |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
16 data points
Data
1 Depth sed [m] | 2 Sample label (DSDP/ODP/IODP sample designation) | 3 Cl [%] (water soluble, Ion chromatogr...) | 4 Cl [%] (structually bound, Ion chroma...) | 5 Cl [%] (total, Ion chromatography) |
---|---|---|---|---|
530.66 | 558-41R-3, 66-69 | 0.15 | <0.01 | 0.15 |
536.99 | 558-42R-1, 99-101 | 0.36 | 0.03 | 0.39 |
545.02 | 558-43Rv1, 2-4 | 0.01 | <0.01 | 0.01 |
557.02 | 558-44R-3, 2-4 | 0.40 | 0.31 | 0.71 |