Emelyanov, Emelyan M (1992): (Table 4) Mineral composition of sediments from Core AMK20-2129 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.759236, In supplement to: Emelyanov, EM (1992): The sediments of the anoxic basins of the Mediterranean Sea. Oceanology, 32(3), 382-388
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 34.297400 * Longitude: 20.014400
Minimum DEPTH, sediment/rock: 0.015 m * Maximum DEPTH, sediment/rock: 5.275 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, top/min | Depth top | m | Emelyanov, Emelyan M | ||
| 3 | Depth, bottom/max | Depth bot | m | Emelyanov, Emelyan M | ||
| 4 | Quartz | Qz | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 5 | Plagioclase | Pl | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 6 | Kalifeldspar | Kfs | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 7 | Illite | Ill | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 8 | Kaolinite | Kln | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 9 | Montmorillonite | Mnt | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 10 | Calcite | Cal | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 11 | Aragonite | Arg | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 12 | Dolomite | Dol | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | |
| 13 | Phases, amorphous to X-ray | XRA | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) | and halite |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
108 data points
Data
| 1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Qz [%] | 5 Pl [%] | 6 Kfs [%] | 7 Ill [%] | 8 Kln [%] | 9 Mnt [%] | 10 Cal [%] | 11 Arg [%] | 12 Dol [%] | 13 XRA [%] |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.015 | 0.00 | 0.03 | 21 | 0 | 6 | 17 | 6 | 6 | 21 | 3 | 13 | 7 |
| 0.775 | 0.75 | 0.80 | 19 | 4 | 9 | 5 | 5 | 6 | 22 | 5 | 9 | 16 |
| 1.325 | 1.30 | 1.35 | 26 | 10 | 6 | 10 | 6 | 5 | 18 | 4 | 8 | 7 |
| 2.525 | 2.50 | 2.55 | 22 | 24 | 11 | 4 | 0 | 4 | 17 | 3 | 7 | 8 |
| 2.630 | 2.61 | 2.65 | 13 | 5 | 23 | 7 | 4 | 5 | 21 | 3 | 8 | 11 |
| 3.000 | 3.00 | 3.00 | 16 | 3 | 0 | 8 | 6 | 7 | 31 | 6 | 2 | 20 |
| 3.775 | 3.75 | 3.80 | 18 | 4 | 0 | 9 | 6 | 4 | 31 | 6 | 4 | 18 |
| 4.325 | 4.30 | 4.35 | 18 | 4 | 0 | 10 | 7 | 8 | 28 | 6 | 5 | 14 |
| 5.275 | 5.25 | 5.30 | 20 | 5 | 3 | 10 | 6 | 5 | 23 | 5 | 4 | 15 |