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Davies, Hugh L; Clarke, J D A; Stagg, Howard M J; McGowran, Brian; Shafik, Samir; Alley, Neville F; Graham, T; Choi, D; Willcox, John Barry (1988): Annotated record of the detailed examination of Mn deposits from the R/V Rig Seismic Cruise 11 (BMR 66) in 1986 over the Great Australian Bight Basin area [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.858474, Supplement to: Davies, HL et al. (1988): Geological results of R/V Rig Seismic Cruise 11, Great Australian Bight Basin 1986. Bureau of Mineral Resources, Geology and Geophysics, Australia, Record 1988/16, 66 pp, Rec1988_016.pdf

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Abstract:
Late Cretaceous and younger sediments dredged from the upper continental slope and canyon walls in the Great Australian Bight Basin between 126° and 136°E broadly confirm the stratigraphy which had been established previously from scattered exploration wells. Late Cretaceous to Early Eocene marine and marginal marine terrigenous sediments are overlain by Middle Eocene and younger pelagic carbonate (fine limestone and calcareous ooze). The samples provide the first evidence of truly marine Maastrichtian sedimentation, with abundant calcareous nannoplankton, on the southern margin of the continent. Other samples of interest include Precambrian sheared granodiorite on the upper slope south of Eyre Terrace, Paleocene phosphatic sediment in 'Eucla' Canyon at 128° 30'E, and terrigenous Early Miocene mudstone at 133° 20' and 134° 50'E. The mudstone is of note as an exception to the uniform pelagic carbonate wackestone and ooze which characterise Middle Eocene and younger sedimentation at all other sites. Fragments of alkali basalt lava of unknown age were recovered in 'Eucla' Canyon. Cores are mostly pelagic calcareous ooze, but those from submarine canyons include terrigenous turbidites.
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:
Median Latitude: -35.206748 * Median Longitude: 134.714174 * South-bound Latitude: -35.730870 * West-bound Longitude: 132.857742 * North-bound Latitude: -34.703776 * East-bound Longitude: 135.589614
Minimum DEPTH, sediment/rock: m * Maximum DEPTH, sediment/rock: m
Event(s):
BMR66-6D (66DR06)  * Latitude: -34.703776 * Longitude: 132.857742 * Elevation: -2015.0 m * Recovery: 50 [kg] * Location: Great Autralian Bight * Campaign: Cruise11-BMR66 * Basis: Rig Seismic * Method/Device: Dredge (DRG)
BMR66-11D (66DR11)  * Latitude: -34.754703 * Longitude: 135.219973 * Elevation: -2141.0 m * Recovery: 40 [kg] * Location: Great Autralian Bight * Campaign: Cruise11-BMR66 * Basis: Rig Seismic * Method/Device: Dredge (DRG)
BMR66-14D (66DR14)  * Latitude: -35.637645 * Longitude: 135.189365 * Elevation: -2627.0 m * Recovery: 35 [kg] * Location: Great Autralian Bight * Campaign: Cruise11-BMR66 * Basis: Rig Seismic * 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
Event labelEventDavies, Hugh L
Latitude of eventLatitudeDavies, Hugh L
Longitude of eventLongitudeDavies, Hugh L
Elevation of eventElevationmDavies, Hugh L
IdentificationIDDavies, Hugh L
DEPTH, sediment/rockDepth sedmDavies, Hugh LGeocode
PositionPositionDavies, Hugh LVisual description
Deposit typeDeposit typeDavies, Hugh L
Quantity of depositQuantityDavies, Hugh L
10 SizeSizeDavies, Hugh L
11 Substrate typeSubstrateDavies, Hugh L
12 Sediment typeSedimentDavies, Hugh L
13 CommentCommentDavies, Hugh L
14 DescriptionDescriptionDavies, Hugh L
Size:
33 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Event

Latitude

Longitude

Elevation [m]

ID

Depth sed [m]

Position

Deposit type

Quantity
10 
Size
11 
Substrate
12 
Sediment
13 
Comment
14 
Description
BMR66-6D -34.70378132.85774-2015BMR66-6D-10SurfaceMn crustSeveralSmallRock; limestone fragmentCalcareous oozeOligocene fine pelagic wackestoneSeveral small fragments of white limestone (foraminiferal spicular wackestone partly replaced by Mn oxides) with a distintive ferruginous and manganiferous weathering crust.
BMR66-11D -34.75470135.21997-2141BMR66-11D-10SurfaceMn coatingSeveralConsolidated sedimentCalcareous oozeWhite chalky ooze (spicular wackestone)Borings/burrows still open and some lined by brown material (iron or manganese oxide) which also coats some other surfaces.
BMR66-14D -35.63764135.18936-2627BMR66-14D-10SurfaceMn stainingSeveralRock; limestoneCalcareous oozeHard white limestone (foraminiferal lime mudstone); well bored; probably represents a hardground surface; iron and manganese staining on surface; stylolites and weak planar layering.
BMR66-15D -35.73087135.58961-2494BMR66-15D-10SurfaceMn crustSeveralLargeRock; mudstoneLime mudstone85 percent is white (5Y8/l) with greenish tinge, soft friable foraminiferal lime mudstone; forms rounded blocksSmall filled and unfilled burrows; exposed surfaces encrusted with manganese oxide and bored.