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Usui, Akira; Nishimura, Akira (1992): Observation of manganese deposits on Kaikata Seamount, Izu-Ogasawara (Bonin) Arc by the Shikai 2000 submersible [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.880486, Supplement to: Usui, A; Nishimura, A (1992): Submersible observations of hydrothermal manganese deposits on the Kaikata Seamount, Izu-Ogasawara (Bonin) Arc. Marine Geology, 106(3-4), 203-216, https://doi.org/10.1016/0025-3227(92)90130-A

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Abstract:
During Dive 408 of Shinkai 2000 on the flank of the Kaikata Seamount located on the volcanic front of the Izu-Ogasawara (Bonin) Arc, possibly recent hydrothermal manganese deposits were observed on sandy volcanic sediments at water depths of between 800 and 1200 m. The deposits cover almost the entire surface sediment across the manganese belt on the northwestern flank on the seamount on a scale of kilometers. The occurrence of the deposits, seafloor morphology and temperature of the sediments, together with previous shipboard results, lead to a possible model for the formation of the manganese deposits: A low-temperature hydrothermal solution ascends through fractures or faults in the volcanic substrate into permeable volcanic sands and precipitates manganate minerals which cement several centimeters of surface sand as hardpan. More intense and probably intermittent discharge of hydrothermal solution follows and forms many typical ridge-like vents and mounds on the seafloor. Subsequently, pure dense manganate layers developed beneath the semi-consolidated volcanic sandstone and act as a cap to the ascending fluids. The proposed mechanism may be the dominant type of low-temperature hydrothermal mineralization in submarine island-arc volcanoes and rifts. Similar hydrothermal manganese deopsits most probably occur in other active areas of the modern seafloors and in inactive island arcs.
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
Coverage:
Median Latitude: 26.702042 * Median Longitude: 140.917666 * South-bound Latitude: 26.701000 * West-bound Longitude: 140.915333 * North-bound Latitude: 26.703167 * East-bound Longitude: 140.919333
Date/Time Start: 1989-06-01T00:00:00 * Date/Time End: 1989-06-01T00:00:00
Minimum DEPTH, sediment/rock: m * Maximum DEPTH, sediment/rock: m
Event(s):
Shinkai2000_408-S1 (DV408/St_1)  * Latitude: 26.703167 * Longitude: 140.915333 * Date/Time: 1989-06-01T00:00:00 * Elevation: -1220.0 m * Location: Kaikata Seamount, Pacific Ocean * Campaign: Shinkai2000_DV408 (Na8906) * Basis: Natsushima * Method/Device: Submersible Shinkai 2000 (S2000) * Comment: Institute: JAMSTEC
Shinkai2000_408-S2 (DV408/St_2)  * Latitude: 26.702167 * Longitude: 140.917833 * Date/Time: 1989-06-01T00:00:00 * Elevation: -1150.0 m * Location: Kaikata Seamount, Pacific Ocean * Campaign: Shinkai2000_DV408 (Na8906) * Basis: Natsushima * Method/Device: Submersible Shinkai 2000 (S2000) * Comment: Institute: JAMSTEC
Shinkai2000_408-S3 (DV408/St_3)  * Latitude: 26.701833 * Longitude: 140.918167 * Date/Time: 1989-06-01T00:00:00 * Elevation: -1167.0 m * Location: Kaikata Seamount, Pacific Ocean * Campaign: Shinkai2000_DV408 (Na8906) * Basis: Natsushima * Method/Device: Submersible Shinkai 2000 (S2000) * Comment: Institute: JAMSTEC
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 labelEventUsui, Akira
Date/Time of eventDate/TimeUsui, Akira
Latitude of eventLatitudeUsui, Akira
Longitude of eventLongitudeUsui, Akira
Elevation of eventElevationmUsui, Akira
Sample IDSample IDUsui, Akira
DEPTH, sediment/rockDepth sedmUsui, AkiraGeocode
PositionPositionUsui, Akira
Deposit typeDeposit typeUsui, Akira
10 Quantity of depositQuantityUsui, Akira
11 SizeSizeUsui, Akira
12 Substrate typeSubstrateUsui, Akira
13 Sediment typeSedimentUsui, Akira
14 DescriptionDescriptionUsui, Akira
15 Uniform resource locator/link to imageURL imageUsui, Akira
Size:
32 data points

Data

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


Event

Date/Time

Latitude

Longitude

Elevation [m]

Sample ID

Depth sed [m]

Position

Deposit type
10 
Quantity
11 
Size
12 
Substrate
13 
Sediment
14 
Description
15 
URL image
Shinkai2000_408-S1 1989-0626.7032140.9153-1220Shikai2000_408-S1-10SurfaceMn coatingSeveralConsolidated sedimentHard groundSlight mineralisation. Top is sandstone like consolidated coarse volcanic sand impregnated with manganese oxides. Fragile frangipan deposit.
Shinkai2000_408-S2 1989-0626.7022140.9178-1150Shikai2000_408-S2-10SurfaceMn coatingSeveralConsolidated sedimentHard groundSlight mineralisation. Top is sandstone like consolidated coarse volcanic sand impregnated with manganese oxides. Fragile frangipan deposit.
Shinkai2000_408-S3 1989-0626.7018140.9182-1167Shikai2000_408-S3-10SurfaceMn crustManyUp to 3.0 cmBasaltHard groundHardpan of manganese impregnated coarse volcanic sand covering dense submetallic pure manganese sheets of a few centimeters (up to 3.0 cm)DV408-St3_Fig9_Usui.jpg
Shinkai2000_408-S4 1989-0626.7010140.9193-1110Shikai2000_408-S4-10SurfaceMn crustManyUp to 10.0 cmBasaltHard groundHardpan of manganese impregnated coarse volcanic sand covering dense submetallic pure thick manganese sheets(3.0-6.0 cm, up to 10.0 cm)DV408-St4_Fig9_Usui.jpg