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Winterhalter, Boris (1966): Annotated record and chemical composition of iron-manganese nodules from the Baltic Sea [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.856728, Supplement to: Winterhalter, B (1966): Pohjanlahden ja Suomenlahden rauta-mangaani-saostumista. Summary: Iron-manganese concretions from the gulf of Bothnia and the gulf of Finland. Geoteknillisiä julkaisuja - Geotekniska meddelanden - Geotechnical publications, 69, 77 pp, https://tupa.gtk.fi/julkaisu/geoteknillinen/gt_s_069.pdf

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Abstract:
Iron-manganese concretions, closely related to lacustrine ores and deep sea manganese nodules, are presently forming in different parts of Gulfs of Bothnia and Finland. They can be divided according to physical form into three distinct groups: (1) round pea-shaped concretions, (2) ring-shaped concrections, and (3) flat sheets and crusts of concretionary material. A definite correlation was found to exist between the form i.e. type of concretions and their chemical composition (Mn/Fe ratio). Trace element concentrations were generally rather high, although not as high as in deep sea manganese nodules. X-ray and DTA was used to study the mineralogy and crystal structure of the concretions. Surface concentrations and geographical distribution of the concretions were estimated on the basis of samples, diving observations and echo-grams.
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
Winterhalter, Boris: Figure 1: Coalesced round iron-manganese concretions from the central part of the Bothnian Bay at station 14RR4. hdl:10013/epic.46576.d001
Winterhalter, Boris: Figure 4: Observation of concretions and their relation to underlying sediment done using SCUBA-equipment down to a depth of 40 meters. hdl:10013/epic.46576.d002
Winterhalter, Boris: Figure 5: Agglomerated concretion (Korso type) fromed by the action of currents and successive partial dissolution and regrowth. hdl:10013/epic.46576.d003
Winterhalter, Boris: Figure 7: Typical disc-shaped flat concretion with a mammilated surface. hdl:10013/epic.46576.d004
Winterhalter, Boris: Figure 8: Round (pea-shaped or grain-like) concretions from sample A7 in the central part of the Gulf of Bothnia. hdl:10013/epic.46576.d005
Winterhalter, Boris: Figure 10a: Side view of a ring-shaped concretion formed around a small granitic pebble. hdl:10013/epic.46576.d006
Coverage:
Median Latitude: 62.469209 * Median Longitude: 22.595586 * South-bound Latitude: 59.583333 * West-bound Longitude: 17.713330 * North-bound Latitude: 65.291670 * East-bound Longitude: 27.391670
Date/Time Start: 1956-01-01T00:00:00 * Date/Time End: 1963-09-07T00:00:00
Comment:
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.
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