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Lalou, Claude; Ku, Teh-Lung; Brichet, Evelyne; Poupeau, G; Romary, P (1979): (Table 1, page 264), Annotated record of the detailed examination of the TECHNO crust [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.855047, In supplement to: Lalou, C et al. (1979): TECHNO encrustation, Part I: Radiometric studies. In: Lalou C. & Sorensen, B.M. (Eds), La Genèse Des Nodules de Manganèse. Centre Océanologique de Bretagne, Gif-sur-Yvette, France, 261-269, hdl:10013/epic.46220.d031

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Coverage:
Latitude: -13.090000 * Longitude: -148.620000
Date/Time Start: 1973-11-03T00:00:00 * Date/Time End: 1973-11-03T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 0.000 m
Event(s):
NX10-CL * Latitude: -13.090000 * Longitude: -148.620000 * Date/Time: 1973-11-03T00:00:00 * Elevation: -4020.0 m * Location: Pacific Ocean * Campaign: NIXO10 (TECHNO 07) * Basis: Marara * Method/Device: Dredge (DRG)
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1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions.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.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1IdentificationIDLalou, Claude
2DEPTH, sediment/rockDepth sedmLalou, ClaudeGeocode
3PositionPositionLalou, ClaudeVisual description
4Deposit typeDeposit typeLalou, Claude
5Quantity of depositQuantityLalou, Claude
6SizeSizeLalou, Claude
7Substrate typeSubstrateLalou, Claude
8Sediment typeSedimentLalou, Claude
9CommentCommentLalou, Claude
10DescriptionDescriptionLalou, Claude
Size:
9 data points

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