Bel'tenev, V E; Shagin, Alexander A; Markov, V F; Rozhdestvenskaya, I I; Lazareva, L I; Fedorov, I P; Cherkashov, Georgy A; Stepanova, Tamara V; Poroshina, Irina M; Shilov, V V (2006): Average contents of chemical elements in different types of hydrothermal manifestations within 16°38'N hydrothermal field, MAR [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.788236, Supplement to: Bel'tenev, VE et al. (2006): New hydrothermal ore field at 16°38'N of the Mid-Atlantic Ridge. Translated from Doklady Akademii Nauk, Ser. Geol., 2006, 408(4), 495-499, Doklady Earth Sciences, 408(4), 530-534, https://doi.org/10.1134/S1028334X06040052
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Abstract:
An additional ore field in the central part of the MARhas been discovered. Together with previously discovered Logachev (14°45'N) and Ashadze (12°58'N) ore fields, the new ore field constitutes a cluster with preliminarily estimated total ore reserve of >10 Mt, which is comparable with large continental massive sulfide deposits.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 16.640000 * Longitude: -46.472500
Event(s):
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
166 data points
Data
1 Rock | 2 NOBS [#] | 3 Fe [%] | 4 Cu [%] | 5 Zn [%] | 6 TS [%] | 7 Mn [%] | 8 Ca [%] | 9 Si [%] | 10 Al [%] | 11 Mg [%] | 12 Pb [%] | 13 Co [%] | 14 Cd [mg/kg] | 15 Au [mg/kg] | 16 Ag [mg/kg] | 17 Ba [mg/kg] | 18 Sb [mg/kg] | 19 Pd [mg/kg] | 20 Pt [ng/kg] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
high-temperature sulfide chimneys | 12 | 38.42 | 3.21 | 0.15 | 43.30 | 0.01 | 0.68 | 0.30 | 0.06 | 0.06 | 0.020 | 0.070 | 14.17 | 0.57 | 15.85 | 271.23 | 21.33 | 0.020 | 200000 |
high-temperature porous sulfides | 14 | 41.58 | 0.28 | 0.26 | 45.42 | 0.01 | 0.41 | 0.13 | 0.06 | 0.05 | 0.040 | 0.040 | 12.50 | 0.90 | 9.14 | 242.57 | 23.78 | 0.021 | 20000 |
high-temperature massive sulfides | 11 | 41.54 | 0.45 | 0.10 | 46.07 | 0.01 | 0.23 | 0.14 | 0.06 | 0.05 | 0.050 | 0.030 | 20.00 | 0.54 | 9.87 | 269.92 | 24.39 | ||
high-temperature massive Fe sulfides (pyrrhotite-pyrite, pyrite) | 35 | 41.25 | 0.33 | 0.18 | 45.34 | 0.01 | 0.45 | 0.18 | 0.06 | 0.05 | 0.040 | 0.040 | 15.10 | 0.69 | 10.24 | 253.60 | 23.30 | ||
high-temperature Cu sulfides (isocubanite-chalcopyrite-pyrite) | 1 | 19.60 | 33.00 | 0.16 | 27.20 | 0.02 | 0.30 | 0.78 | 0.12 | 0.05 | 0.060 | 0.100 | 30.00 | 1.03 | 60.00 | 46.00 | 18.10 | ||
high-temperature veinlet-disseminated mineralization in basalts | 5 | 27.05 | 0.23 | 0.02 | 30.26 | 0.01 | 0.20 | 17.55 | 0.05 | 0.05 | 0.020 | 0.090 | 6.00 | 0.47 | 9.26 | 177.28 | 21.50 | ||
low-temperature veinlet-disseminated mineralization in sediments | 3 | 36.87 | 0.56 | 0.56 | 1.70 | 0.01 | 1.63 | 5.02 | 1.39 | 0.76 | 0.060 | 0.020 | 11.67 | 1.03 | 6.33 | 22208.30 | 25.13 | ||
low-temperature oxide-hydroxide crusts | 7 | 44.44 | 1.61 | 0.41 | 0.50 | 0.04 | 0.66 | 3.91 | 0.34 | 0.38 | 0.060 | 0.020 | 18.57 | 0.14 | 3.94 | 3916.80 | 30.36 | ||
low-temperature siliceous material | 1 | 4.15 | 0.01 | 0.15 | 1.63 | 0.01 | 2.10 | 35.53 | 0.10 | 0.13 | 0.012 | 0.008 | 5.00 | 0.17 | 3.80 | 27700.00 | 19.90 |