Robinson, Paul T; Thayer, Julie A; Cook, Peter J; McKnight, Brian K (1974): Annotated record of the detailed examination of Mn deposits from DSDP Leg 27 (Sites 259, 261, 263) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.869312, Supplement to: Robinson, PT et al. (1974): Lithology of Mesozoic and Cenozoic Sediments of the Eastern Indian Ocean, Leg 27, Deep Sea Drilling Project. In: Veevers, J.J.; Heirtzler, J.R.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXVII, 1001-1047, https://doi.org/10.2973/dsdp.proc.27.148.1974
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Abstract:
During Leg 27 five sites were drilled in the eastern Indian Ocean, four in abyssal plains near the western margin of Australia and one in the Timor Trough. Abyssal plain sediments are divided into two major units: (1) a lower, acoustically transparent layer of relatively uniform thickness draped over basaltic basement and (2) a horizontally layered sequence of highly variable thickness filling low areas on the surface of the transparent layer. The transparent layer, ranging in age from Upper Jurassic to Upper Cretaceous, consists chiefly of dark gray, siliceous clays and claystones with minor zeolitic clay and nannofossil ooze. Sedimentation rates are between 5 and 30 m/m.y. being highest in the Lower Cretaceous. Upper Cretaceous sediment are sparse or absent. The relatively high sedimentation rates for pelagic clay are probably due to the proximity of the Australian continent. The layered unit consists of calcareous oozes and lesser zeolitic clay and radiolarian ooze, all of Cenozoic age. Many of the oozes contain shallow-water foraminifers and graded sequences suggesting deposition by mass transport.
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
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: -21.962833 * Median Longitude: 113.850833 * South-bound Latitude: -29.617500 * West-bound Longitude: 110.963500 * North-bound Latitude: -12.947200 * East-bound Longitude: 117.892700
Date/Time Start: 1972-11-03T00:00:00 * Date/Time End: 1972-12-01T00:00:00
Minimum DEPTH, sediment/rock: 19.81 m * Maximum DEPTH, sediment/rock: 701.09 m
Event(s):
27-259 * Latitude: -29.617500 * Longitude: 112.696300 * Date/Time: 1972-11-03T00:00:00 * Elevation: -4696.0 m * Penetration: 346 m * Recovery: 248.8 m * Campaign: Leg27 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 40 cores; 336.5 m cored; 9.5 m drilled; 73.9 % recovery
27-261 * Latitude: -12.947200 * Longitude: 117.892700 * Date/Time: 1972-11-17T00:00:00 * Elevation: -5667.0 m * Penetration: 579.5 m * Recovery: 120.5 m * Location: Indian Ocean//PLAIN * Campaign: Leg27 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 36 cores; 323 m cored; 9.5 m drilled; 37.3 % recovery
27-263 * Latitude: -23.323800 * Longitude: 110.963500 * Date/Time: 1972-12-01T00:00:00 * Elevation: -5048.0 m * Penetration: 746 m * Recovery: 166.8 m * Location: Indian Ocean//PLAIN * Campaign: Leg27 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 29 cores; 271 m cored; 0 m drilled; 61.5 % recovery
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):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Robinson, Paul T | |||
2 | Identification | ID | Robinson, Paul T | |||
3 | Sample code/label | Sample label | Robinson, Paul T | |||
4 | DEPTH, sediment/rock | Depth sed | m | Robinson, Paul T | Geocode | |
5 | Position | Position | Robinson, Paul T | Visual description | ||
6 | Deposit type | Deposit type | Robinson, Paul T | |||
7 | Quantity of deposit | Quantity | Robinson, Paul T | |||
8 | Size | Size | Robinson, Paul T | |||
9 | Substrate type | Substrate | Robinson, Paul T | |||
10 | Sediment type | Sediment | Robinson, Paul T | |||
11 | Comment | Comment | Robinson, Paul T | |||
12 | Description | Description | Robinson, Paul T |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
66 data points
Data
1 Event | 2 ID | 3 Sample label | 4 Depth sed [m] | 5 Position | 6 Deposit type | 7 Quantity | 8 Size | 9 Substrate | 10 Sediment | 11 Comment | 12 Description |
---|---|---|---|---|---|---|---|---|---|---|---|
27-259 | 27-259-3-2,80-1 | 27-259-3-2,80 | 19.81 | In sediment | Mn micronodule | Few | Clay | Zeolitic clay (Quaternary) | 2% Mn micronodules. ( Site 259, Core 4, Cored Interval: 17.5-27.0 m, page 30 ) | ||
27-259 | 27-259-4-3,50-150-1 | 27-259-4-3,50-150 | 31.40 | In sediment | Mn micronodule | Several | Ooze | Light-orange to light-brown, interbedded, nanno ooze, nanno clay, and zeolite clay (Lower Eocene) | Quartz, forams, and micarb fragments with traces of sponge spicules, fish remains, silico-flagellates, and black micronodules. ( Site 259, Core 4, Cored Interval 27-36.5 m, Page 31 ) | ||
27-259 | 27-259-4-3,50-150-1 | 27-259-4-3,50-150 | 31.40 | Buried | Mn nodule | Many | 0.5-2.0 cm | Ooze | Light-orange to light-brown, interbedded, nanno ooze, nanno clay, and zeolite clay (Lower Eocene) | Numerous small nodules (0.5 to 2 cm). Some nodules are dark gray to black, possibly manganese or iron oxide in composition. ( Site 259, Core 4, Cored Interval 27-36.5 m, Page 31 ) | |
27-261 | 27-261-7-CC,0-1 | 27-261-7-CC,0 | 185.10 | In sediment | Mn micronodule | Several | Clay | Nanno bearing clay (Upper cretaceous) | 20% Mn micronodules in coarse fraction. ( Site 261, Core 7, Cored Interval 180.5-190 m, page 147 ) | ||
27-261 | 27-261-8-CC,0-1 | 27-261-8-CC,0 | 199.10 | In sediment | Mn micronodule | Many | Clay | Zeolitic claystone (Upper cretaceous) | 85% Mn micronodules in coarse fraction. ( Site 261, Core 8, Cored Interval -190-199.5 m, page 148 ) | ||
27-261 | 27-261-9-CC,0-1 | 27-261-9-CC,0 | 205.60 | In sediment | Mn micronodule | Many | Clay | Claystone (Cretaceous) | 30% Mn micronodules in coarse fraction. ( Site 261, Core 9, Cored Interval 199.5-209.0 m, page 148 ) | ||
27-261 | 27-261-15-1,33-1 | 27-261-15-1,33 | 256.83 | In sediment | Mn micronodule | Few | Clay | Calcareous claystone (Lower Cretaceous) | Few Mn micronodules. ( Site 261, Core 15, Cored Interval 256.5-266.0 m, page 140 ) | ||
27-263 | 27-263-26-2,108-110-1 | 27-263-26-2,108-110 | 701.09 | Buried | Mn staining | 1 | Belemnite | Clay | Nanno bearing clay (Lower Cretaceous) | Belemnite guard, coated with a closely adherent layer of clay, apparently impregnated with manganese oxides. ( Site 263, Core 26, Cored Interval: 698.5-708 m, page 306 ) |