Bogdanov, Yury A; Lisitzin, Alexander P; Sagalevich, Anatoly M; Gurvich, Evgeny G (2006): (Table 94) Mineral and chemical compositions of surficial sulfide deposits of a 10 m high hydrothermal mound in the North Lau Basin polygon [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.746467, In supplement to: Bogdanov, YA et al. (2006): Hydrothermal Ore Genesis of the Ocean Floor. Nauka Publ. (Moscow): in Russian, 527 pp
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: -15.390800 * Longitude: -174.668800
Event(s):
AMK21-2226 * Latitude: -15.390800 * Longitude: -174.668800 * Location: Lau Basin * Campaign: AMK21 * Basis: Akademik Mstislav Keldysh * Method/Device: MIR deep-sea manned submersible (MIR)
Comment:
Mineral contents of crystal phase.
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
155 data points
Data
1 Sample label | 2 Samp type | 3 Cv [%] | 4 Ccp [%] | 5 Py [%] | 6 Mrc [%] | 7 Sp [%] | 8 Brt [%] | 9 TS [%] | 10 SiO2 [%] | 11 Al2O3 [%] | 12 Fe [%] | 13 Cu [%] | 14 Zn [%] | 15 Mn [mg/kg] | 16 P [mg/kg] | 17 Pb [mg/kg] | 18 Cd [mg/kg] | 19 As [mg/kg] | 20 Ag [mg/kg] | 21 In [mg/kg] | 22 Ni [mg/kg] | 23 Co [mg/kg] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2226-7 | 0 | 70 | 9 | 6 | 2 | 12 | 1.0 | 12.02 | 0.02 | 20.5 | 18.1 | 1.5 | 140 | 120 | 280 | 12 | 260 | 7.5 | 44.0 | 9 | 68 | |
2226-8 | 0 | 21 | 23 | 1 | 53 | 0 | 2.0 | 0.10 | 0.35 | 22.5 | 4.6 | 17.9 | 45 | 10 | 230 | 320 | 140 | 7.0 | 49.0 | 2 | 56 | |
2226-9 | inner part | 1 | 87 | 0 | 0 | 12 | 0 | 0.2 | 0.58 | 0.18 | 23.0 | 31.6 | 6.2 | 15 | 10 | 110 | 100 | 14.0 | 185.0 | 6 | 78 | |
2226-9 | outer part | 2 | 50 | 0 | 0 | 48 | 0 | 0.3 | 1.39 | 0.21 | 12.7 | 22.6 | 27.4 | 120 | 50 | 220 | 450 | 52.0 | 26.0 | 3 | 51 | |
2226-10 | inner part | 1 | 84 | 0 | 0 | 15 | 0 | 0.0 | 0.58 | 0.11 | 22.0 | 31.2 | 6.5 | 37 | 10 | 130 | 120 | 9.0 | 200.0 | 9 | 130 | |
2226-10 | outer part | 3 | 25 | 6 | 20 | 39 | 7 | 0.0 | 8.70 | 0.02 | 15.0 | 17.8 | 17.2 | 490 | 150 | 620 | 230 | 300 | 42.0 | 30.0 | 3 | 43 |
2226-11 | 0 | 20 | 34 | 0 | 45 | 0 | 1.0 | 0.10 | 0.21 | 24.0 | 3.7 | 13.5 | 60 | 10 | 230 | 220 | 440 | 3.5 | 4.2 | 2 | 29 |