Heft, Kerri L; Gillis, Kathryn M; Pollock, Meagen A; Karson, Jeffrey A; Klein, Emily M (2008): (Table S3) Plagioclase compositions of Pito Deep samples [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.782655, In supplement to: Heft, KL et al. (2008): Role of upwelling hydrothermal fluids in the development of alteration patterns at fast spreading ridges: Evidence from the sheeted dike complex at Pito Deep. Geochemistry, Geophysics, Geosystems, 9, Q05O07, https://doi.org/10.1029/2007GC001926
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Coverage:
Median Latitude: -22.930072 * Median Longitude: -111.957586 * South-bound Latitude: -22.983000 * West-bound Longitude: -112.069000 * North-bound Latitude: -22.873000 * East-bound Longitude: -111.875000
Minimum DEPTH, sediment/rock: 0 m * Maximum DEPTH, sediment/rock: 0 m
Event(s):
Al-4075 * Latitude Start: -22.880000 * Longitude Start: -112.069000 * Latitude End: -22.879000 * Longitude End: -112.067000 * Elevation Start: -3956.0 m * Elevation End: -3622.0 m * Location: Western Pacific * Campaign: AT11-23 * Basis: Atlantis (1997) * Method/Device: Submersible Alvin (ALVIN)
Al-4076 * Latitude Start: -22.883000 * Longitude Start: -112.061000 * Latitude End: -22.883000 * Longitude End: -112.061000 * Elevation Start: -3625.0 m * Elevation End: -3575.0 m * Location: Western Pacific * Campaign: AT11-23 * Basis: Atlantis (1997) * Method/Device: Submersible Alvin (ALVIN)
Al-4077 * Latitude Start: -22.886000 * Longitude Start: -112.051000 * Latitude End: -22.882000 * Longitude End: -112.046000 * Elevation Start: -3575.0 m * Elevation End: -3199.0 m * Location: Western Pacific * Campaign: AT11-23 * Basis: Atlantis (1997) * Method/Device: Submersible Alvin (ALVIN)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Heft, Kerri L | |||
| 3 | Area/locality | Area | Heft, Kerri L | |||
| 4 | Depth, bathymetric | Bathy depth | m | Heft, Kerri L | ||
| 5 | Latitude of event | Latitude | ||||
| 6 | Longitude of event | Longitude | ||||
| 7 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 8 | Depth, relative | Depth rel | m | Heft, Kerri L | below lava-dike transitio | |
| 9 | Lithology/composition/facies | Lithology | Heft, Kerri L | |||
| 10 | Silicon dioxide | SiO2 | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 11 | Titanium dioxide | TiO2 | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 12 | Aluminium oxide | Al2O3 | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 13 | Iron oxide, FeO | FeO | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 14 | Manganese oxide | MnO | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 15 | Magnesium oxide | MgO | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 16 | Calcium oxide | CaO | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 17 | Sodium oxide | Na2O | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 18 | Potassium oxide | K2O | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 19 | Elements, total | Total | % | Heft, Kerri L | Electron microprobe (EMP) | |
| 20 | Silicon | Si | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 21 | Titanium | Ti | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 22 | Aluminium | Al | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 23 | Iron 2+ and 3+ | Fe | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 24 | Manganese | Mn | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 25 | Magnesium | Mg | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 26 | Calcium | Ca | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 27 | Sodium | Na | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 28 | Potassium | K | # of ions | Heft, Kerri L | Calculated based on oxygen number | |
| 29 | Anorthite | An | % | Heft, Kerri L | Calculated based on oxygen number |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
7411 data points
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