Astakhova, N V; Sorochinskaya, A V (2001): (Table 2) Chemical composition of carbonate and barite tubes and nodules and bulk sediments from Core AS-9310 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.762364, In supplement to: Astakhova, NV; Sorochinskaya, AV (2001): Hydrothermal formations in the Deryugin Basin sediments of the Sea of Okhotsk. Translated from Okeanologiya, 2001, 41(3), 447-455, Oceanology, 41(3), 429-437
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 54.011700 * Longitude: 146.283300
Minimum DEPTH, sediment/rock: 0.25 m * Maximum DEPTH, sediment/rock: 1.27 m
Event(s):
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
117 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 Lab no | 5 SiO2 [%] | 6 Fe2O3 [%] | 7 Al2O3 [%] | 8 MnO [%] | 9 CaO [%] | 10 MgO [%] | 11 Na2O [%] | 12 K2O [%] | 13 BaO [%] | 14 CO2 [%] | 15 Zn [mg/kg] | 16 Ni [mg/kg] | 17 Cu [mg/kg] | 18 Sr [mg/kg] | 19 Ag [mg/kg] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.25 | 0.20 | 0.30 | carbonate nodule | 40.33 | 4.68 | 4.28 | 0.152 | 13.160 | 0.752 | 1.220 | 1.010 | 13.00 | 6.41 | 130.0 | 185.0 | 109.0 | 1340 | |
0.35 | 0.10 | 0.60 | barite nodule | 38.60 | 4.67 | 4.62 | 0.132 | 12.830 | 0.406 | 0.990 | 1.130 | 14.71 | 81.6 | 122.0 | 194.0 | 1630 | ||
0.45 | 0.40 | 0.50 | carbonate tubes | 59.22 | 2.50 | 6.26 | 0.226 | 11.260 | 0.914 | 1.180 | 1.260 | 3.70 | 19.11 | 140.0 | 140.0 | 52.5 | 960 | 26.25 |
0.45 | 0.40 | 0.50 | sediment | 67.13 | 5.28 | 12.00 | 0.185 | 0.602 | 0.815 | 3.150 | 2.120 | 4.84 | 123.0 | 123.0 | 61.5 | 102 | ||
0.90 | 0.85 | 0.95 | carbonate nodule | 23.18 | 4.32 | 2.13 | 0.150 | 30.800 | 0.415 | 2.630 | 0.630 | 8.78 | 9.49 | 120.0 | 120.0 | 42.0 | 250 | |
0.94 | 0.60 | 1.28 | barite tubes | 46.85 | 5.06 | 2.95 | 0.106 | 0.770 | 0.233 | 0.587 | 0.709 | 22.30 | 240.0 | 51.2 | 64.0 | 1600 | ||
1.27 | 1.26 | 1.28 | sediment | 47.80 | 5.38 | 12.52 | 0.178 | 0.608 | 0.787 | 3.520 | 2.290 | 17.00 | 138.0 | 198.0 | 20.0 | 90 | 19.78 |