Emelyanov, Emelyan M (1998): (Table II.12.2) Mineral composition of bottom sediments from Core AMK20-2129 collected in the Bannock Basin [dataset]. P.P. Shirshov Institute of Oceanology, RAS, Atlantic Branch, Kaliningrad, PANGAEA, https://doi.org/10.1594/PANGAEA.772225, In supplement to: Emelyanov, EM (1998): Bar'ernye Zony v Okeane (Barrier Zones in the Ocean). Yantarny Skaz (Kaliningrad), 416 pp
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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) | and strontianite |
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 |
14 | Sum | Sum | % | Emelyanov, Emelyan M | X-ray diffraction (XRD) |
License:
Creative Commons Attribution-NonCommercial 3.0 Unported (CC-BY-NC-3.0)
Size:
117 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 [%] | 14 Sum [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.015 | 0.00 | 0.03 | 21 | 0 | 6 | 17 | 6 | 6 | 21 | 3 | 13 | 7 | 100 |
0.775 | 0.75 | 0.80 | 19 | 4 | 9 | 5 | 5 | 6 | 22 | 5 | 9 | 16 | 100 |
1.325 | 1.30 | 1.35 | 26 | 10 | 6 | 10 | 6 | 5 | 18 | 4 | 8 | 7 | 100 |
2.530 | 2.50 | 2.56 | 22 | 24 | 11 | 4 | 0 | 4 | 17 | 3 | 7 | 8 | 100 |
2.630 | 2.61 | 2.65 | 13 | 5 | 23 | 7 | 4 | 5 | 21 | 3 | 8 | 11 | 100 |
3.030 | 3.00 | 3.06 | 17 | 3 | 0 | 9 | 6 | 8 | 33 | 0 | 2 | 22 | 100 |
3.775 | 3.75 | 3.80 | 18 | 4 | 0 | 9 | 6 | 4 | 31 | 6 | 4 | 18 | 100 |
4.325 | 4.30 | 4.35 | 18 | 4 | 0 | 10 | 7 | 8 | 28 | 6 | 5 | 14 | 100 |
5.275 | 5.25 | 5.30 | 20 | 5 | 3 | 10 | 6 | 5 | 27 | 5 | 4 | 15 | 100 |