Volkov, Igor I (1984): (Table 6.5) Sulfir isotopic composition of sulfide nodules from the Anatolian slope of the Black Sea [dataset]. P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, PANGAEA, https://doi.org/10.1594/PANGAEA.771752, In supplement to: Volkov, II (1984): Geokhimiya Sery v Osadkakh Okeana (Geochemistry of Sulfur in Ocean Sediments). Nauka Publ. (Moscow): in Russian, 272 pp
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 41.556333 * Median Longitude: 37.858000 * South-bound Latitude: 41.233333 * West-bound Longitude: 34.908333 * North-bound Latitude: 42.280000 * East-bound Longitude: 41.171667
Minimum DEPTH, sediment/rock: 0.070 m * Maximum DEPTH, sediment/rock: 0.150 m
Event(s):
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 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
6 | Depth, top/min | Depth top | m | Volkov, Igor I | ||
7 | Depth, bottom/max | Depth bot | m | Volkov, Igor I | ||
8 | Minerals | Minerals | Volkov, Igor I | |||
9 | δ34S | δ34S | ‰ CDT | Volkov, Igor I | Mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
24 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth sed [m] | 6 Depth top [m] | 7 Depth bot [m] | 8 Minerals | 9 δ34S [‰ CDT] |
---|---|---|---|---|---|---|---|---|
IV84-1635 | 42.280 | 34.908 | -1015 | 0.085 | 0.01 | 0.16 | pyrite | -26.2 |
IV84-1665 | 41.425 | 37.417 | -1030 | 0.095 | 0.02 | 0.17 | melnikovite | -15.0 |
IV84-1666-I | 41.233 | 37.897 | -400 | 0.070 | 0.02 | 0.12 | pyrite | -26.8 |
IV84-1666-II | 41.233 | 37.897 | -340 | 0.150 | 0.10 | 0.20 | melnikovite | 16.6 |
IV84-1679 | 41.610 | 41.172 | -1295 | 0.105 | 0.01 | 0.20 | pyrite | -33.0 |
IV84-1679 | 41.610 | 41.172 | -1295 | 0.105 | 0.01 | 0.20 | melnikovite | -22.0 |