McManus, Dean A; Burns, Robert E (2005): Smear slide analysis of Hole 5-42 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230777
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
Milow, E Dean; Goll, Robert M; Olsson, Richard K; von der Borch, Christopher C; Vallier, Tracy L; Weser, Oscar E; Burns, Robert E; McManus, Dean A (1970): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, V, 827 pp, https://doi.org/10.2973/dsdp.proc.5.1970
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 13.842700 * Longitude: -140.188500
Date/Time Start: 1969-05-26T00:00:00 * Date/Time End: 1969-05-26T00:00:00
Minimum DEPTH, sediment/rock: 0.69 m * Maximum DEPTH, sediment/rock: 98.90 m
Event(s):
5-42 * Latitude: 13.842700 * Longitude: -140.188500 * Date/Time: 1969-05-26T00:00:00 * Elevation: -4848.0 m * Penetration: 100 m * Recovery: 90.6 m * Location: North Pacific/HILL * Campaign: Leg5 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 100 m cored; 0 m drilled; 90.6 % 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 | Spiculae | Spiculae | % | Smear slide analysis | ||
14 | Zeolite | Zeo | % | Smear slide analysis | ||
15 | Clay minerals | Clay min | % | Smear slide analysis | ||
16 | Volcanic glass | Volc glass | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1185 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 Spiculae [%] | 14 Zeo [%] | 15 Clay min [%] | 16 Volc glass [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.69 | 5-42-1-1,69 | 0 | 8 | 92 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
1.80 | 5-42-1-2,30 | 0 | 40 | 60 | Upper oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 45 | 0 | 0 | 0 | 0 | 0 | 15 | 2 |
2.15 | 5-42-1-2,65 | 0 | 15 | 85 | Upper oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
2.84 | 5-42-1-21,134 | 0 | 8 | 92 | Upper oligocene | NANNO CHALK OOZE | Minor lithology; numerical abundance | 92 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
5.70 | 5-42-1-41,120 | 0 | 5 | 95 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 95 | 0 | 5 | 0 | 2 | 0 | 2 | 0 |
7.19 | 5-42-1-51,119 | 0 | 15 | 85 | Upper oligocene | RAD NANNO CHALK OOZE | Minor lithology; relative abundance | 85 | 0 | 15 | 0 | 0 | 0 | 2 | 0 |
8.53 | 5-42-1-61,103 | 0 | 2 | 98 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 98 | 0 | 2 | 0 | 0 | 0 | 2 | 0 |
9.10 | 5-42-2-1,10 | 0 | 10 | 90 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 90 | 0 | 5 | 0 | 0 | 0 | 2 | 5 |
9.80 | 5-42-2-1,80 | 0 | 5 | 95 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 92 | 0 | 5 | 0 | 0 | 0 | 2 | 0 |
11.25 | 5-42-2-2,75 | 0 | 5 | 95 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 95 | 0 | 5 | 0 | 2 | 0 | 2 | 0 |
13.00 | 5-42-2-31,100 | 0 | 5 | 95 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 95 | 0 | 5 | 0 | 0 | 0 | 2 | 0 |
13.95 | 5-42-2-4,45 | 0 | 15 | 85 | Upper oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 85 | 0 | 15 | 0 | 0 | 0 | 2 | 0 |
14.52 | 5-42-2-41,102 | 0 | 10 | 90 | Upper oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 90 | 0 | 10 | 0 | 0 | 0 | 2 | 0 |
15.55 | 5-42-2-5,55 | 0 | 10 | 90 | Upper oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 90 | 0 | 10 | 0 | 0 | 0 | 2 | 0 |
17.00 | 5-42-2-6,50 | 0 | 15 | 85 | Upper oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 85 | 0 | 15 | 0 | 0 | 0 | 2 | 2 |
18.00 | 5-42-3-1,0 | 0 | 8 | 92 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 92 | 0 | 8 | 0 | 2 | 0 | 2 | 2 |
27.60 | 5-42-4-1,60 | 0 | 100 | 0 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 75 | 0 | 25 | 0 | 0 | 0 | 2 | 2 |
29.42 | 5-42-4-2,92 | 0 | 100 | 0 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 80 | 0 | 20 | 0 | 0 | 0 | 0 | 2 |
29.80 | 5-42-4-21,130 | 0 | 95 | 5 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 75 | 0 | 20 | 0 | 2 | 0 | 5 | 2 |
30.75 | 5-42-4-3,75 | 0 | 20 | 80 | Lower oligocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 80 | 0 | 20 | 0 | 2 | 0 | 2 | 2 |
31.10 | 5-42-4-31,110 | 5 | 85 | 10 | Lower oligocene | RAD OOZE | Minor lithology; relative abundance | 0 | 0 | 20 | 0 | 2 | 0 | 10 | 2 |
31.85 | 5-42-4-4,35 | 5 | 90 | 5 | Lower oligocene | NANNO RAD OOZE | Dominat lithology; relative abundance | 30 | 0 | 60 | 0 | 5 | 0 | 5 | 2 |
32.60 | 5-42-4-41,110 | 5 | 90 | 5 | Lower oligocene | RAD OOZE | Minor lithology; relative abundance | 5 | 0 | 85 | 0 | 5 | 0 | 5 | 2 |
33.75 | 5-42-4-5,75 | 5 | 90 | 5 | Lower oligocene | NANNO RAD OOZE | Dominat lithology; relative abundance | 20 | 0 | 70 | 0 | 5 | 0 | 5 | 2 |
34.16 | 5-42-4-51,116 | 0 | 12 | 88 | Lower oligocene | RAD NANNO CHALK OOZE | Minor lithology; relative abundance | 88 | 0 | 12 | 0 | 0 | 0 | 2 | 0 |
35.32 | 5-42-4-6,82 | 0 | 100 | 0 | Upper eocene | NANNO RAD OOZE | Dominat lithology; relative abundance | 45 | 0 | 55 | 0 | 0 | 0 | 2 | 2 |
37.60 | 5-42-5-1,60 | 0 | 95 | 5 | Upper eocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 95 | 0 | 0 | 0 | 0 | 0 | 5 | 2 |
38.00 | 5-42-5-11,100 | 0 | 95 | 5 | Upper eocene | RAD OOZE | Minor lithology; relative abundance | 2 | 0 | 95 | 0 | 0 | 0 | 5 | 0 |
39.70 | 5-42-5-21,120 | 5 | 90 | 5 | Upper eocene | NANNO RAD OOZE | Minor lithology; numerical abundance | 40 | 0 | 50 | 0 | 5 | 0 | 5 | 0 |
40.50 | 5-42-5-3,50 | 0 | 95 | 5 | Upper eocene | RAD OOZE | Dominat lithology; relative abundance | 2 | 0 | 95 | 0 | 0 | 0 | 5 | 0 |
43.95 | 5-42-5-5,95 | 0 | 95 | 5 | Upper eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 0 | 0 | 0 | 5 | 2 |
44.95 | 5-42-5-6,45 | 0 | 90 | 10 | Upper eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 0 | 0 | 0 | 10 | 0 |
46.32 | 5-42-6-1,32 | 0 | 100 | 0 | Upper eocene | RAD NANNO CHALK OOZE | Minor lithology; relative abundance | 85 | 0 | 15 | 0 | 0 | 0 | 2 | 0 |
47.45 | 5-42-6-11,145 | 0 | 100 | 0 | Upper eocene | INDURATED ASH | Minor lithology; numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 95 |
47.49 | 5-42-6-11,149 | 0 | 95 | 5 | Upper eocene | RAD OOZE | Dominat lithology; numerical abundance | 10 | 0 | 85 | 0 | 0 | 0 | 5 | 0 |
48.00 | 5-42-6-2,50 | 0 | 95 | 5 | Upper eocene | NANNO RAD OOZE | Dominat lithology; numerical abundance | 35 | 0 | 60 | 0 | 0 | 0 | 5 | 0 |
48.80 | 5-42-6-21,130 | 0 | 100 | 0 | Upper eocene | RAD NANNO CHALK OOZE | Minor lithology; relative abundance | 55 | 0 | 45 | 0 | 0 | 0 | 2 | 0 |
49.30 | 5-42-6-3,30 | 0 | 100 | 0 | Upper eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 60 | 0 | 40 | 0 | 0 | 0 | 2 | 0 |
50.10 | 5-42-6-31,110 | 0 | 100 | 0 | Upper eocene | NANNO RAD OOZE | Minor lithology; relative abundance | 40 | 0 | 60 | 0 | 0 | 0 | 2 | 0 |
51.33 | 5-42-6-4,83 | 0 | 100 | 0 | Upper eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 55 | 0 | 45 | 0 | 0 | 0 | 2 | 0 |
52.80 | 5-42-6-5,80 | 0 | 100 | 0 | Upper eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 65 | 0 | 35 | 0 | 0 | 0 | 2 | 0 |
54.40 | 5-42-6-6,90 | 0 | 100 | 0 | Upper eocene | NANNO RAD OOZE | Dominat lithology; relative abundance | 35 | 0 | 65 | 0 | 0 | 0 | 2 | 0 |
58.00 | 5-42-7-21,150 | 0 | 100 | 0 | Upper eocene | NANNO RAD OOZE | Dominat lithology; relative abundance | 40 | 0 | 60 | 0 | 0 | 0 | 2 | 0 |
60.38 | 5-42-7-4,88 | 0 | 95 | 5 | Upper eocene | RAD OOZE | Dominat lithology; numerical abundance | 5 | 0 | 90 | 0 | 0 | 0 | 5 | 0 |
60.40 | 5-42-7-4,90 | 0 | 100 | 0 | Upper eocene | RAD NANNO OOZE | Minor lithology; relative abundance | 80 | 0 | 20 | 0 | 0 | 0 | 2 | 0 |
60.52 | 5-42-7-41,102 | 0 | 95 | 5 | Upper eocene | NANNO RAD OOZE | Minor lithology; numerical abundance | 35 | 0 | 60 | 0 | 0 | 0 | 5 | 0 |
62.50 | 5-42-7-51,150 | 0 | 95 | 5 | Upper eocene | RAD OOZE | Dominat lithology; numerical abundance | 5 | 0 | 90 | 0 | 0 | 0 | 5 | 0 |
64.00 | 5-42-7-61,150 | 0 | 100 | 0 | Middle eocene | NANNO RAD OOZE | Dominat lithology; relative abundance | 35 | 0 | 65 | 0 | 0 | 0 | 2 | 0 |
64.37 | 5-42-8-1,37 | 0 | 95 | 5 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 60 | 2 | 35 | 0 | 0 | 0 | 5 | 0 |
65.30 | 5-42-8-11,130 | 0 | 95 | 5 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 60 | 0 | 35 | 0 | 0 | 0 | 5 | 0 |
67.00 | 5-42-8-21,150 | 0 | 100 | 0 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 60 | 0 | 40 | 0 | 0 | 0 | 2 | 0 |
67.60 | 5-42-8-3,60 | 20 | 15 | 65 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 65 | 2 | 35 | 2 | 2 | 0 | 2 | 0 |
67.66 | 5-42-8-3,66 | 20 | 20 | 60 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 60 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
69.60 | 5-42-8-41,110 | 25 | 10 | 65 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 65 | 0 | 35 | 0 | 0 | 0 | 0 | 0 |
70.58 | 5-42-8-5,58 | 10 | 5 | 85 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 85 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
71.45 | 5-42-8-51,145 | 0 | 100 | 0 | Middle eocene | ALTERED VOLCANICS | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 75 |
73.00 | 5-42-8-61,150 | 0 | 95 | 5 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 60 | 0 | 35 | 0 | 0 | 0 | 5 | 0 |
73.50 | 5-42-9-1,50 | 10 | 10 | 80 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 80 | 0 | 20 | 0 | 0 | 0 | 2 | 0 |
73.64 | 5-42-9-1,64 | 20 | 20 | 60 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 60 | 0 | 20 | 0 | 0 | 0 | 2 | 0 |
75.75 | 5-42-9-21,125 | 0 | 90 | 10 | Middle eocene | NANNO RAD OOZE | Dominat lithology; numerical abundance | 35 | 0 | 55 | 0 | 0 | 0 | 10 | 0 |
76.82 | 5-42-9-3,82 | 30 | 25 | 45 | Middle eocene | NANNO RAD OOZE | Dominat lithology; relative abundance | 40 | 0 | 55 | 0 | 0 | 0 | 5 | 2 |
77.05 | 5-42-9-31,105 | 0 | 95 | 5 | Middle eocene | NANNO RAD OOZE | Dominat lithology; numerical abundance | 20 | 0 | 75 | 0 | 0 | 0 | 5 | 0 |
77.70 | 5-42-9-4,20 | 10 | 20 | 70 | Middle eocene | RAD NANNO CHALK OOZE | Minor lithology; relative abundance | 70 | 0 | 30 | 0 | 0 | 0 | 2 | 0 |
78.22 | 5-42-9-4,72 | 0 | 90 | 10 | Middle eocene | NANNO RAD OOZE | Dominat lithology; numerical abundance | 15 | 0 | 75 | 0 | 0 | 0 | 10 | 0 |
78.81 | 5-42-9-41,131 | 0 | 95 | 0 | Middle eocene | VOLCANIC ASH | Minor lithology; relative abundance | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 95 |
80.10 | 5-42-9-51,110 | 0 | 90 | 10 | Middle eocene | NANNO RAD OOZE | Dominat lithology; numerical abundance | 20 | 0 | 70 | 0 | 0 | 0 | 10 | 0 |
81.40 | 5-42-9-6,90 | 0 | 90 | 10 | Middle eocene | NANNO RAD OOZE | Dominat lithology; numerical abundance | 30 | 0 | 60 | 0 | 0 | 0 | 10 | 0 |
81.75 | 5-42-9-61,125 | 0 | 90 | 10 | Middle eocene | NANNO RAD OOZE | Dominat lithology; numerical abundance | 40 | 0 | 50 | 0 | 0 | 0 | 10 | 0 |
82.71 | 5-42-10-1,71 | 45 | 40 | 15 | Middle eocene | RAD OOZE | Minor lithology; relative abundance | 2 | 0 | 85 | 0 | 0 | 0 | 15 | 0 |
83.20 | 5-42-10-11,120 | 20 | 20 | 60 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 60 | 0 | 20 | 0 | 0 | 0 | 2 | 0 |
84.13 | 5-42-10-2,63 | 20 | 20 | 60 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 50 | 0 | 40 | 0 | 0 | 0 | 10 | 0 |
84.63 | 5-42-10-21,113 | 15 | 15 | 70 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 70 | 0 | 30 | 0 | 0 | 0 | 0 | 0 |
87.20 | 5-42-10-4,70 | 20 | 20 | 60 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 60 | 0 | 20 | 0 | 0 | 0 | 2 | 0 |
90.20 | 5-42-10-6,70 | 0 | 90 | 10 | Middle eocene | NANNO RAD OOZE | Minor lithology; numerical abundance | 40 | 0 | 50 | 0 | 0 | 0 | 10 | 0 |
90.30 | 5-42-10-6,80 | 0 | 95 | 5 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; numerical abundance | 60 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
92.76 | 5-42-11-1,76 | 25 | 10 | 65 | Middle eocene | RAD NANNO CHALK OOZE | Dominat lithology; relative abundance | 65 | 0 | 35 | 0 | 0 | 0 | 2 | 0 |
94.97 | 5-42-11-21,147 | 35 | 35 | 30 | Middle eocene | NANNO RAD OOZE | Dominat lithology; relative abundance | 25 | 0 | 35 | 0 | 0 | 0 | 5 | 0 |
98.15 | 5-42-11-5,15 | 30 | 30 | 40 | Middle eocene | NANNO RAD OOZE | Minor lithology; relative abundance | 40 | 0 | 60 | 0 | 0 | 0 | 0 | 2 |
98.90 | 5-42-11-5,90 | 0 | 0 | 0 | Middle eocene | RAD NANNO OOZE | Dominat lithology; numerical abundance | 68 | 0 | 33 | 0 | 0 | 0 | 0 | 0 |