McManus, Dean A; Burns, Robert E (2005): Smear slide analysis of Hole 5-40 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230775
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:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 19.792800 * Longitude: -139.901300
Date/Time Start: 1969-05-20T00:00:00 * Date/Time End: 1969-05-20T00:00:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 143.30 m
Event(s):
5-40 * Latitude: 19.792800 * Longitude: -139.901300 * Date/Time: 1969-05-20T00:00:00 * Elevation: -5183.0 m * Penetration: 156 m * Recovery: 130.6 m * Location: North Pacific/BASIN * Campaign: Leg5 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 18 cores; 144 m cored; 9 m drilled; 90.7 % 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 | Minerals, other | Min other | % | Smear slide analysis | ||
15 | Feldspar | Fsp | % | Smear slide analysis | ||
16 | Zeolite | Zeo | % | Smear slide analysis | ||
17 | Clay minerals | Clay min | % | Smear slide analysis | ||
18 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
19 | Fecal pellets | Fecal pel | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1242 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 Min other [%] | 15 Fsp [%] | 16 Zeo [%] | 17 Clay min [%] | 18 Volc glass [%] | 19 Fecal pel [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.02 | 5-40-1-1,2 | 0 | 50 | 50 | Neogene | ZOELITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 15 | 6 | 36 | 50 | 6 | 0 |
0.40 | 5-40-1-1,40 | 0 | 40 | 60 | Neogene | ZEOLITIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 30 | 60 | 0 | 0 |
0.78 | 5-40-1-1,78 | 0 | 50 | 50 | Neogene | ZEOLITIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 40 | 50 | 0 | 0 |
0.86 | 5-40-1-1,86 | 0 | 55 | 45 | Neogene | ZEOLITIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 50 | 45 | 0 | 0 |
0.93 | 5-40-1-1,93 | 0 | 55 | 45 | Neogene | ZEOLITIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 45 | 45 | 0 | 0 |
2.42 | 5-40-1-2,92 | 0 | 100 | 1 | Neogene | CLAY BEARING ZEOLITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 90 | 2 | 0 | 0 |
2.50 | 5-40-1-21,100 | 0 | 45 | 55 | Neogene | ZEOLITE CLAY | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 10 | 0 | 35 | 55 | 0 | 0 |
3.75 | 5-40-1-3,75 | 0 | 50 | 50 | Neogene | ZEOLITIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 40 | 50 | 0 | 0 |
3.92 | 5-40-1-3,92 | 0 | 50 | 50 | Neogene | ZEOLITIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 45 | 50 | 0 | 0 |
5.50 | 5-40-1-41,100 | 0 | 45 | 55 | Neogene | ZEOLITIC CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 40 | 55 | 0 | 0 |
6.98 | 5-40-1-5,98 | 0 | 90 | 10 | Neogene | ZEOLITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 92 | 10 | 0 | 0 |
8.56 | 5-40-1-61,106 | 0 | 90 | 10 | Neogene | ZEOLITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 90 | 10 | 0 | 0 |
8.75 | 5-40-1-61,125 | 0 | 45 | 55 | Neogene | ZEOLITIC RED CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 40 | 55 | 2 | 0 |
9.00 | 5-40-1-61,150 | 0 | 30 | 70 | Neogene | ZEOLITIC RED CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 25 | 70 | 0 | 0 |
9.05 | 5-40-2-1,5 | 20 | 60 | 20 | Neogene | SILICEOUS FOSSIL DEVIT. VOLCANIC ASH | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 40 | 0 |
9.10 | 5-40-1-CC,0 | 0 | 2 | 0 | Neogene | ZEOLITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 98 | 0 | 0 | 0 |
9.16 | 5-40-2-1,16 | 0 | 60 | 40 | Neogene | ZEOLITIC RED CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 60 | 40 | 0 | 0 |
9.85 | 5-40-2-1,85 | 30 | 30 | 60 | Neogene | CLAYEY RAD OOZE | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 |
11.00 | 5-40-2-2,50 | 25 | 25 | 50 | Upper eocene | CLAYEY RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 |
11.90 | 5-40-2-21,140 | 30 | 20 | 50 | Upper eocene | CLAYEY RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 |
12.75 | 5-40-2-3,75 | 35 | 30 | 35 | Upper eocene | RED CLAY RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 55 | 6 | 4 | 0 | 0 | 0 | 35 | 0 | 0 |
14.25 | 5-40-2-4,75 | 50 | 45 | 5 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
16.10 | 5-40-2-51,110 | 65 | 35 | 1 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 95 | 5 | 0 | 0 | 0 | 2 | 0 | 0 |
17.30 | 5-40-2-6,80 | 35 | 25 | 40 | Middle eocene | RED CLAY RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 |
18.10 | 5-40-2-CC,0 | 20 | 80 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 |
19.50 | 5-40-3-11,150 | 55 | 42 | 3 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 |
20.25 | 5-40-3-2,75 | 55 | 45 | 5 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
20.68 | 5-40-3-21,118 | 50 | 50 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
27.00 | 5-40-4-1,0 | 0 | 100 | 0 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 20 | 2 |
27.10 | 5-40-3-CC,0 | 0 | 100 | 1 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
28.50 | 5-40-4-11,150 | 50 | 50 | 1 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
31.50 | 5-40-4-31,150 | 50 | 45 | 5 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
34.50 | 5-40-4-51,150 | 55 | 45 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
37.50 | 5-40-5-11,150 | 50 | 47 | 3 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 |
38.24 | 5-40-5-2,74 | 50 | 50 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
39.75 | 5-40-5-3,75 | 50 | 50 | 1 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
45.00 | 5-40-5-61,150 | 52 | 48 | 1 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
51.00 | 5-40-6-21,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
52.20 | 5-40-6-31,120 | 5 | 90 | 5 | Middle eocene | VOLCANIC ASH | Minor lithology; relative abundance | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 5 | 80 | 0 |
54.00 | 5-40-6-41,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
55.50 | 5-40-6-51,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
57.00 | 5-40-6-61,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
57.10 | 5-40-6-CC,0 | 0 | 95 | 5 | Middle eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 0 | 0 | 2 | 0 | 0 | 5 | 2 | 0 |
67.50 | 5-40-8-11,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
69.00 | 5-40-8-21,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
69.75 | 5-40-8-3,75 | 55 | 40 | 5 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
72.00 | 5-40-8-41,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
75.00 | 5-40-8-61,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
78.00 | 5-40-9-21,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
82.50 | 5-40-9-51,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
87.00 | 5-40-10-21,150 | 100 | 0 | 0 | Middle eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
90.00 | 5-40-10-41,150 | 100 | 0 | 0 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
96.00 | 5-40-11-21,150 | 100 | 0 | 0 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
98.74 | 5-40-11-41,124 | 50 | 45 | 5 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
98.77 | 5-40-11-41,127 | 50 | 50 | 0 | Lower eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
102.00 | 5-40-11-61,150 | 100 | 0 | 0 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
105.00 | 5-40-12-21,150 | 100 | 0 | 0 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
109.50 | 5-40-12-51,150 | 100 | 0 | 0 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
113.40 | 5-40-13-11,140 | 50 | 50 | 1 | Lower eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 2 | 2 | 0 | 0 | 0 | 2 | 0 | 0 |
124.75 | 5-40-14-3,75 | 50 | 45 | 5 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
132.03 | 5-40-15-2,53 | 5 | 95 | 0 | Lower eocene | PUMICE-VOLCANIC GLASS FRAGMENT | Minor lithology; relative abundance | 0 | 0 | 1 | 0 | 0 | 5 | 0 | 0 | 2 | 95 | 0 |
133.10 | 5-40-15-3,10 | 0 | 20 | 80 | Lower eocene | RED CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 80 | 0 | 0 |
133.75 | 5-40-15-3,75 | 50 | 50 | 1 | Lower eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
135.25 | 5-40-15-4,75 | 50 | 50 | 1 | Lower eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
135.60 | 5-40-15-41,110 | 50 | 45 | 5 | Lower eocene | RAD OOZE | Dominat lithology; relative abundance | 0 | 0 | 95 | 2 | 2 | 0 | 0 | 0 | 5 | 0 | 0 |
139.90 | 5-40-16-1,90 | 50 | 45 | 5 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
142.31 | 5-40-16-3,31 | 50 | 45 | 5 | Lower eocene | RAD OOZE | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
142.70 | 5-40-16-3,70 | 0 | 20 | 80 | Lower eocene | ZEOLITE BEARING RED CLAY | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 80 | 0 | 0 |
143.30 | 5-40-16-31,130 | 30 | 50 | 20 | Lower eocene | CLAYEY RAD OOZE | Minor lithology; relative abundance | 0 | 0 | 80 | 2 | 2 | 0 | 0 | 0 | 20 | 0 | 0 |