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Bonatti, Enrico; Joensuu, Oiva (1966): (Table 1, page 643) Spectrochemical analyses of samples from dredge haul AMPHITRITE D2. Three different fragments of red ferruginous rock [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.854408, Supplement to: Bonatti, E; Joensuu, O (1966): Deep-Sea Iron Deposit from the South Pacific. Science, 154(3749), 643-645, https://doi.org/10.1126/science.154.3749.643

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Published: 1966 (exact date unknown)DOI registered: 2015-11-24

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Abstract:
Along with specimens of manganese oxides and basalt, rocks containing more than 30 percent iron by weight and consisting mainly of poorly crystallized goethite have been dredged from the flanks of a seamount located on the East Pacific Rise. The Fe-Mn ratio varies widely among the various oxide rocks deposited at this locality and at another seamount in the same area. The deposit was probably formed by fractional precipitation of iron and manganese which had been introduced locally into the bottom water by hydrothermal solutions of volcanic origin, and by leaching from deep-sea basaltic lavas.
Source:
Grant, John Bruce; Moore, Carla J; Alameddin, George; Chen, Kuiying; Barton, Mark (1992): The NOAA and MMS Marine Minerals Geochemical Database. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V52Z13FT
Further details:
Warnken, Robin R; Virden, William T; Moore, Carla J (1992): The NOAA and MMS Marine Minerals Bibliography. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V53X84KN
Coverage:
Latitude: -10.633000 * Longitude: -109.600000
Date/Time Start: 1963-12-23T00:00:00 * Date/Time End: 1963-12-23T00:00:00
Minimum DEPTH, sediment/rock: m * Maximum DEPTH, sediment/rock: m
Event(s):
AMPH-002D (AMPH01AR-002D) * Latitude: -10.633000 * Longitude: -109.600000 * Date/Time: 1963-12-23T00:00:00 * Elevation: -3256.0 m * Location: Pacific Ocean * Campaign: AMPHITRITE (AMPH01AR) * Basis: Argo * Method/Device: Dredge (DRG) * Comment: PI: Von Herzen, Richard P.
Comment:
Percent H2O indicates the loss in weight of the moisture-free sample after 24 hours at 600°C.
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample IDSample IDBonatti, Enrico
2DEPTH, sediment/rockDepth sedmBonatti, EnricoGeocode
3Silicon dioxideSiO2%Bonatti, EnricoOptical spectrographic analysis
4Aluminium oxideAl2O3%Bonatti, EnricoOptical spectrographic analysis
5Calcium oxideCaO%Bonatti, EnricoOptical spectrographic analysis
6Magnesium oxideMgO%Bonatti, EnricoOptical spectrographic analysis
7Potassium oxideK2O%Bonatti, EnricoOptical spectrographic analysis
8IronFe%Bonatti, EnricoOptical spectrographic analysis
9ManganeseMn%Bonatti, EnricoOptical spectrographic analysis
10NickelNimg/kgBonatti, EnricoOptical spectrographic analysis
11CobaltComg/kgBonatti, EnricoOptical spectrographic analysis
12ChromiumCrmg/kgBonatti, EnricoOptical spectrographic analysis
13CopperCumg/kgBonatti, EnricoOptical spectrographic analysis
14BariumBamg/kgBonatti, EnricoOptical spectrographic analysis
15BoronBmg/kgBonatti, EnricoOptical spectrographic analysis
16StrontiumSrmg/kgBonatti, EnricoOptical spectrographic analysis
17Loss on dryingLOD%Bonatti, EnricoH2O loss
Size:
46 data points

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