Pimm, Anthony C (1974): Annotated record of the detailed examination of Mn deposits from DSDP Leg 22 (Sites 212, 213, 215, 216, 217, 217A) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.869093, Supplement to: Pimm, AC (1974): Sedimentology and History of the Northeastern Indian Ocean from Late Cretaceous to Recent. In: von der Borch, C.C.; Sclater, J.G.; et al., Initial Reports of the Deep Sea Drilling Project, Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XXII, 717-803, https://doi.org/10.2973/dsdp.proc.22.139.1974
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Abstract:
Eight sites were drilled on Leg 22 in the northeastern Indian Ocean. Three sites (214, 216, 217) on Ninetyeast Ridge penetrated a thick sequence of mostly Tertiary calcareous oozes passing down into shallow-water sediments with volcanogenic material in Sites 214 and 216. The age of the basal sequence increases northwards from Paleocene (214) through Maastrichtian (216) to Campanian (217). A nonmarine sequence of volcanoclastics and lignite overlies basalt at 214. Drilling terminated in a dolomite chert sequence at 217 before bsalt was encountered. Two sites (213, 215), in deep water on either side of Ninetyeast Ridge, showed calcareous ooze of Paleocene to early Eocene age overlying basalt passing up into brown clay and finally siliceous ooze of late Miocene and younger age. A major hiatus centered in the Oligocene occurs at both these sites. One site (212), drilled in the deepest part of the Wharton Basin, penetrated a brown clay sequence interbedded with several thick calcareous units, each of a very short time duration. Evidence from sedimentary structures and calcareous microfossils.
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: -3.034650 * Median Longitude: 91.878467 * South-bound Latitude: -19.189000 * West-bound Longitude: 86.791700 * North-bound Latitude: 8.926200 * East-bound Longitude: 99.297300
Date/Time Start: 1972-01-27T00:00:00 * Date/Time End: 1972-02-24T00:00:00
Minimum DEPTH, sediment/rock: 5.09 m * Maximum DEPTH, sediment/rock: 508.52 m
Event(s):
22-212 * Latitude: -19.189000 * Longitude: 99.297300 * Date/Time: 1972-01-27T00:00:00 * Elevation: -6233.0 m * Penetration: 521 m * Recovery: 171.2 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 38 cores; 355 m cored; 0 m drilled; 48.2 % recovery
22-213 * Latitude: -10.211800 * Longitude: 93.896200 * Date/Time: 1972-02-04T00:00:00 * Elevation: -5601.0 m * Penetration: 163 m * Recovery: 143.6 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 163 m cored; 0 m drilled; 88.1 % recovery
22-215 * Latitude: -8.121700 * Longitude: 86.791700 * Date/Time: 1972-02-13T00:00:00 * Elevation: -5309.0 m * Penetration: 175 m * Recovery: 116 m * Location: Indian Ocean//BASIN * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 20 cores; 175 m cored; 0 m drilled; 66.3 % 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 | ||||
2 | Identification | ID | ||||
3 | Sample code/label | Sample label | ||||
4 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
5 | Position | Position | Visual description | |||
6 | Deposit type | Deposit type | ||||
7 | Quantity of deposit | Quantity | ||||
8 | Size | Size | ||||
9 | Substrate type | Substrate | ||||
10 | Sediment type | Sediment | ||||
11 | Comment | Comment | ||||
12 | Description | Description |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
122 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 |
---|---|---|---|---|---|---|---|---|---|---|---|
22-212 | 22-212-10-1,25-1 | 22-212-10-1,25 | 164.75 | In sediment | Mn micronodule | Many | Clay | Iron oxide rich clay (Middle Miocene) | 25% Mn micronodules. ( Site 212, Core 10, Cored interval 164.5-174.0 m, page 50 ) | ||
22-212 | 22-212-16-1,80-1 | 22-212-16-1,80 | 298.30 | In sediment | Mn micronodule | Many | Clay | Zeolite-bearing iron-oxide-rich claystone (Eocene) | 30% Mn micronodules. ( Site 212, Core 16, Cored interval 297.5-307.0 m, page 53 ) | ||
22-212 | 22-212-29-0,16-1 | 22-212-29-0,16 | 421.16 | In sediment | Mn micronodule | Several | Clay | Clay-bearing to essentially pure (>95% nannofossils) nannofossil chalk (Upper cretaceous) | Volcanic glass and manganese micronodules comprise a significant admixture to the nannofossils. ( Site 212, Core 29, Cored interval 421-430.5 m, page 58 ) | ||
22-212 | 22-212-38-2,52-1 | 22-212-38-2,52 | 508.52 | In sediment | Mn micronodule | Several | Clay | Iron rich claystone 15% Mn nodules | 15% Mn micronodules. ( Site 212, Core 38, Cored interval 506.5-516.0 m, page 62 ) | ||
22-213 | 22-213-1-4,39-1 | 22-213-1-4,39 | 5.09 | In sediment | Mn micronodule | Several | Clay | Manganese clay with radiolarian rich diatom ooze (Quaternary) | 14% Mn micronodules. ( Site 213, Core 1, Cored interval 0-9 m, page 93 ) | ||
22-213 | 22-213-2-2,60-1 | 22-213-2-2,60 | 11.10 | In sediment | Mn micronodule | Several | Ash | Volcanic ash clay manganese bearing radiolarian rich diatom ooze (Quaternary) | 10% Mn micronodules. ( Site 213, Core 2, Cored interval 9-18.5 m, page 93 ) | ||
22-213 | 22-213-12-61,115-1 | 22-213-12-61,115 | 112.65 | In sediment | Mn micronodule | Several | Clay | Manganese iron oxide mineral rich clay | 10% Mn micronodules. ( Site 213, Core 12, Cored interval 9-18.5 m, page 98 ) | ||
22-213 | 22-213-16-41,145-1 | 22-213-16-41,145 | 147.95 | In sediment | Mn micronodule | Many | Clay | Clay rich iron oxide (Upper Paleocene) | 80% Mn micronodules. ( Site 213, Core 16, Cored interval 142-151.5 m, page 100 ) | ||
22-213 | 22-213-17-2,0-1 | 22-213-17-2,0 | 152.00 | Buried | Mn coating | Several | Rock; basalt | Basalt | A succession of at least 11 basaltic flows | Each flow is a pillow-lava with chilled margins, 80% Mn micronodules. ( Site 213, Core 17, Cored interval 151.5-159.5 m, page 101 ) | |
22-215 | 22-215-9-1,48-1 | 22-215-9-1,48 | 74.48 | In sediment | Mn micronodule | Several | Clay | Zeolite Mn-Fe rich clay (Lower Eocene) | 10% Mn micronodule. ( Site 215, Core 9, Cored interval 74-83.5 m, page 204 ) | ||
22-215 | 22-215-17-11,100-1 | 22-215-17-11,100 | 151.00 | In sediment | Mn micronodule | Several | Clay | Iron oxide rich clay, nanno ooze (Paleocene) | 12% Mn micronodule. ( Site 215, Core 17, Cored interval 150-155.5 m, page 208 ) | ||
22-216 | 22-216-20-1,90-1 | 22-216-20-1,90 | 301.90 | In sediment | Mn micronodule | Several | Chalk | Nanno chalk white (N9), also light olive gray 5Y6/1 and grayish orange pink (5YR7/2)(Paleocene) | Mn micronodules and specks. ( Site 216, Core 20, Cored interval 301-310.5 m, page 227 ) | ||
22-216 | 22-216-21-11,120-1 | 22-216-21-11,120 | 311.70 | In sediment | Mn micronodule | Several | Chalk | Pink white ooze chert with white chalk (Paleocene) | Mn micronodules in gray laminae. ( Site 216, Core 21, Cored interval 310.5-320 m, page 227 ) | ||
22-217 | 22-217-14-1,10-1 | 22-217-14-1,10 | 392.60 | In sediment | Mn micronodule | Several | Up to 0.5 cm | Chalk | Foram bearing nanno chalk (Middle Paleocene) | With some Mn micronodules (<5 mm). ( Site 217, Core 14, Cored interval 392.5-402 m, page 282 ) | |
22-217A | 22-217A-2-3,80-1 | 22-217A-2-3,80 | 13.30 | In sediment | Mn micronodule | Several | Clay | Foram bearing clay, rich in nanno ooze (Quaternary) | Some darker layers with specs of black Mn. ( Site 217A, Core 2, Cored interval 9.5-19 m, page 293 ) |