van Andel, Tjeerd H; Heath, G Ross (2005): Smear slide analysis of Hole 16-157A. PANGAEA, https://doi.org/10.1594/PANGAEA.230397
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
DSDP (1989): Data from the Deep Sea Drilling Project. Sediment, hard rock and reference files. National Geophysical Data Center, National Environmental Satellite, Data and Information Service, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1, CD-ROM
Yeats, Robert S; Rodolfo, Kelvin S; Kaneps, Ansis G; Dinkelman, Menno G; Cronan, David S; Charleston, Santiago; Bukry, David; Bennett, Richard H; van Andel, Tjeerd H; Heath, G Ross (1973): Initial Reports of the Deep Sea Drilling Project 16. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XVI, 949 pp, https://doi.org/10.2973/dsdp.proc.16.1973
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -1.761700 * Longitude: -85.902800
Date/Time Start: 1971-02-12T00:00:00 * Date/Time End: 1971-02-12T00:00:00
Minimum DEPTH, sediment/rock: 1.00 m * Maximum DEPTH, sediment/rock: 26.29 m
Event(s):
16-157A * Latitude: -1.761700 * Longitude: -85.902800 * Date/Time: 1971-02-12T00:00:00 * Elevation: -2591.0 m * Penetration: 27 m * Recovery: 19.3 m * Location: South Pacific/RIDGE * Campaign: Leg16 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 3 cores; 27 m cored; 0 m drilled; 71.5 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Sample code/label | Sample label | DSDP/ODP/IODP sample designation | |||
3 | Sand | Sand | % | Smear slide analysis | ||
4 | Silt | Silt | % | Smear slide analysis | ||
5 | Size fraction < 0.002 mm, clay | <2 µm | % | Smear slide analysis | ||
6 | Stratigraphy | Stratigraphy | Smear slide analysis | |||
7 | Lithology/composition/facies | Lithology | Smear slide analysis | |||
8 | Comment | Comment | Smear slide analysis | |||
9 | Nannofossils | Nannos | % | Smear slide analysis | ||
10 | Foraminifera | Foram | % | Smear slide analysis | ||
11 | Radiolarians | Rad | % | Smear slide analysis | ||
12 | Diatoms | Diatoms | % | Smear slide analysis | ||
13 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
14 | Spiculae | Spiculae | % | Smear slide analysis | ||
15 | Quartz | Qz | % | Smear slide analysis | ||
16 | Palagonite | Palagonite | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
330 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Nannos [%] | 10 Foram [%] | 11 Rad [%] | 12 Diatoms [%] | 13 Silicoflag [%] | 14 Spiculae [%] | 15 Qz [%] | 16 Palagonite [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.00 | 16-157A-1-11,100 | 0 | 0 | 0 | Quaternary | NANNO FORAM CHALK OOZE | Dominat lithology; numerical abundance | 29 | 29 | 12 | 29 | 1 | 0 | 0 | 0 |
1.40 | 16-157A-1-11,140 | 0 | 0 | 0 | Quaternary | NANNO FORAM CHALK OOZE | Dominat lithology; relative abundance | 55 | 55 | 1 | 0 | 0 | 0 | 0 | 0 |
1.60 | 16-157A-1-2,10 | 0 | 0 | 0 | Quaternary | NANNO FORAM CHALK OOZE | Dominat lithology; relative abundance | 55 | 55 | 0 | 1 | 0 | 0 | 0 | 0 |
1.75 | 16-157A-1-2,25 | 0 | 0 | 0 | Quaternary | NANNO FORAM CHALK OOZE | Dominat lithology; relative abundance | 55 | 55 | 0 | 1 | 0 | 0 | 0 | 0 |
3.80 | 16-157A-1-3,80 | 0 | 0 | 0 | Quaternary | NANNO FORAM CHALK OOZE | Dominat lithology; relative abundance | 55 | 55 | 1 | 1 | 0 | 0 | 0 | 0 |
4.64 | 16-157A-1-4,14 | 0 | 0 | 0 | Quaternary | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 |
4.64 | 16-157A-1-4,14 | 0 | 0 | 0 | Quaternary | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 |
5.80 | 16-157A-1-41,130 | 0 | 0 | 0 | Quaternary | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 55 | 0 | 0 | 0 | 0 | 0 | 0 |
6.80 | 16-157A-1-5,80 | 0 | 0 | 0 | Quaternary | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 |
7.30 | 16-157A-1-51,130 | 0 | 0 | 0 | Quaternary | NANNO FORAMS CHALK OOZE | Dominat lithology; relative abundance | 55 | 55 | 0 | 23 | 0 | 0 | 0 | 0 |
8.60 | 16-157A-1-61,110 | 0 | 0 | 0 | Quaternary | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 1 | 0 | 0 | 0 | 0 |
8.80 | 16-157A-1-61,130 | 0 | 0 | 0 | Quaternary | NANNO FORAMS CHALK OOZE | Dominat lithology; numerical abundance | 35 | 35 | 14 | 14 | 1 | 0 | 1 | 0 |
9.30 | 16-157A-2-1,30 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 29 | 29 | 12 | 29 | 0 | 0 | 0 | 0 |
9.90 | 16-157A-2-1,90 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 |
10.40 | 16-157A-2-11,140 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 |
19.20 | 16-157A-3-11,120 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 29 | 29 | 12 | 29 | 1 | 0 | 0 | 1 |
19.90 | 16-157A-3-2,40 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 1 | 1 | 1 | 1 | 0 | 0 |
20.90 | 16-157A-3-21,140 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 1 | 1 | 23 | 1 | 0 | 0 |
22.10 | 16-157A-3-31,110 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 23 | 0 | 1 | 1 | 1 | 0 | 0 |
23.70 | 16-157A-3-41,120 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 1 | 1 | 1 | 0 | 0 |
24.60 | 16-157A-3-5,60 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 1 | 1 | 1 | 0 | 0 |
26.29 | 16-157A-3-6,79 | 0 | 0 | 0 | Upper pleistocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 1 | 0 | 23 | 1 | 1 | 0 | 0 |