Maxwell, Arthur E; von Herzen, Richard P (2005): Smear slide analysis of Hole 3-20C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230582
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
Maxwell, Arthur E; Milow, E Dean; Andrews, James E; Hsü, Kenneth J; Von Herzon, Richard P; Boyce, Robert E; Percival, Stephen F Jr; Saito, Tsunemasa (1970): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, III, 806 pp, https://doi.org/10.2973/dsdp.proc.3.1970
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: -28.524500 * Longitude: -26.845500
Date/Time Start: 1969-01-09T00:00:00 * Date/Time End: 1969-01-09T00:00:00
Minimum DEPTH, sediment/rock: 2.15 m * Maximum DEPTH, sediment/rock: 74.70 m
Event(s):
3-20C * Latitude: -28.524500 * Longitude: -26.845500 * Date/Time: 1969-01-09T00:00:00 * Elevation: -4506.0 m * Penetration: 72.3 m * Recovery: 48.6 m * Location: South Atlantic/VALLEY * Campaign: Leg3 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 7 cores; 50.5 m cored; 0 m drilled; 96.2 % 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 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Nannofossils | Nannos | % | Smear slide analysis | ||
12 | Foraminifera | Foram | % | Smear slide analysis | ||
13 | Minerals, other | Min other | % | Smear slide analysis | ||
14 | Quartz | Qz | % | Smear slide analysis | ||
15 | Feldspar | Fsp | % | Smear slide analysis | ||
16 | Zeolite | Zeo | % | Smear slide analysis | ||
17 | Clay minerals | Clay min | % | Smear slide analysis | ||
18 | Iron | Fe | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
824 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Carb [%] | 10 Dol [%] | 11 Nannos [%] | 12 Foram [%] | 13 Min other [%] | 14 Qz [%] | 15 Fsp [%] | 16 Zeo [%] | 17 Clay min [%] | 18 Fe [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
2.15 | 3-20C-1-2,65 | 0 | 1 | 100 | Upper oligocene | RED CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 2 | 80 | 17 |
2.97 | 3-20C-1-21,147 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 2 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
3.40 | 3-20C-1-3,40 | 0 | 1 | 100 | Upper oligocene | ZEOLITE CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 30 | 69 | 0 |
3.75 | 3-20C-1-3,75 | 0 | 0 | 1 | Upper oligocene | PURE NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
4.20 | 3-20C-1-31,120 | 0 | 0 | 1 | Upper oligocene | ZEOLITE RED CLAY | Dominat lithology; numerical abundance | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 35 | 54 | 10 |
5.25 | 3-20C-1-4,75 | 0 | 0 | 10 | Upper oligocene | NANNO CHALK OOZE SLIGHTLY MARLY | Dominat lithology; numerical abundance | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 | 5 | 5 |
5.60 | 3-20C-1-41,110 | 0 | 0 | 30 | Upper oligocene | MARLY NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 0 | 2 | 0 | 0 | 5 | 15 | 0 |
6.75 | 3-20C-1-5,75 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 90 | 0 | 2 | 2 | 0 | 1 | 5 | 4 |
8.00 | 3-20C-1-6,50 | 0 | 0 | 0 | Upper oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 92 | 0 | 0 | 2 | 0 | 1 | 5 | 2 |
9.10 | 3-20C-1-CC,0 | 0 | 0 | 0 | ZEOLITE MARLY NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 10 | 5 | 5 | |
24.60 | 3-20C-2-1,0 | 0 | 0 | 100 | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
27.60 | 3-20C-2-3,0 | 0 | 0 | 0 | Lower oligocene | PURE NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 2 | 0 | 2 |
29.25 | 3-20C-2-4,15 | 0 | 1 | 100 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
29.60 | 3-20C-2-4,50 | 0 | 0 | 0 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
30.16 | 3-20C-2-41,106 | 0 | 0 | 0 | Lower oligocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.60 | 3-20C-2-5,0 | 0 | 1 | 100 | Lower oligocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
33.70 | 3-20C-2-CC,0 | 0 | 1 | 100 | Lower oligocene | PURE NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 2 | 0 | 0 | 0 | 0 | 0 | 2 |
36.90 | 3-20C-3-1,0 | 0 | 0 | 0 | Upper eocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 15 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
38.40 | 3-20C-3-2,0 | 0 | 0 | 0 | Middle eocene | MARLY NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 2 | 0 | 10 |
41.40 | 3-20C-3-4,0 | 0 | 0 | 35 | Middle eocene | MARLY NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 2 | 0 | 5 |
42.65 | 3-20C-3-41,125 | 0 | 0 | 0 | Middle eocene | MARLY NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 10 |
45.15 | 3-20C-3-6,75 | 0 | 0 | 0 | Middle eocene | MARLY NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 80 | 0 | 0 | 0 | 0 | 1 | 0 | 5 |
46.00 | 3-20C-3-CC,0 | 0 | 0 | 0 | Middle eocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 93 | 0 | 0 | 0 | 0 | 0 | 8 | 0 |
47.35 | 3-20C-4-1,75 | 0 | 0 | 0 | Middle eocene | MARLY NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 2 | 15 | 8 |
48.60 | 3-20C-4-2,50 | 0 | 0 | 26 | Middle eocene | MARLY NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 74 | 0 | 0 | 0 | 0 | 1 | 20 | 5 |
49.26 | 3-20C-4-21,116 | 0 | 0 | 0 | Middle eocene | NANNO CHALK | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
49.95 | 3-20C-4-3,35 | 0 | 0 | 100 | Middle eocene | NANNO ZEOLITE CLAY | Dominat lithology; numerical abundance | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 50 | 25 | 10 |
50.35 | 3-20C-4-3,75 | 0 | 0 | 0 | Middle eocene | NANNO CHALK OOZE SLIGHTLY MARLY | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 1 | 4 | 0 |
52.70 | 3-20C-4-CC,0 | 0 | 0 | 100 | Middle eocene | PURE NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
57.00 | 3-20C-5-1,0 | 0 | 1 | 100 | Middle eocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 98 | 2 | 0 | 0 | 0 | 2 | 2 | 2 |
59.02 | 3-20C-5-2,52 | 0 | 0 | 0 | Middle eocene | MARLY NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 2 | 80 | 0 | 0 | 0 | 0 | 0 | 15 | 5 |
59.25 | 3-20C-5-2,75 | 0 | 0 | 0 | Middle eocene | NANNO CHALK | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
60.00 | 3-20C-5-3,0 | 0 | 0 | 0 | Middle eocene | NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
62.25 | 3-20C-5-4,75 | 0 | 0 | 0 | Lower eocene | PURE NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 1 | 1 | 1 |
62.25 | 3-20C-5-4,75 | 0 | 0 | 0 | Lower eocene | PURE NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 98 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
63.75 | 3-20C-5-5,75 | 0 | 2 | 98 | Lower eocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 97 | 2 | 0 | 0 | 0 | 0 | 1 | 0 |
65.25 | 3-20C-5-6,75 | 0 | 1 | 99 | Upper paleocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 98 | 1 | 0 | 0 | 0 | 0 | 1 | 0 |
66.10 | 3-20C-5-CC,0 | 0 | 3 | 97 | Upper paleocene | NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 95 | 3 | 0 | 0 | 0 | 0 | 2 | 0 |
69.35 | 3-20C-6-2,75 | 0 | 0 | 0 | Lower paleocene | PURE NANNO CHALK | Dominat lithology; numerical abundance | 0 | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
69.65 | 3-20C-6-21,105 | 0 | 5 | 95 | Lower paleocene | DOLOMITE NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 5 | 95 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
70.10 | 3-20C-6-3,0 | 0 | 1 | 99 | Lower paleocene | PURE NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 98 | 1 | 0 | 0 | 0 | 0 | 1 | 0 |
71.90 | 3-20C-6-4,30 | 0 | 0 | 100 | Maestrichtian | ALMOST PURE NANNO OOZE | Dominat lithology; numerical abundance | 0 | 0 | 95 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
72.22 | 3-20C-6-4,62 | 0 | 1 | 100 | PARTIALLY RECRYSTALLIZED NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 78 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | |
72.80 | 3-20C-6-41,120 | 0 | 3 | 97 | PARTIALLY RECRYSTALLIZED NANNO CHALK | Dominat lithology; relative abundance | 0 | 2 | 72 | 3 | 0 | 0 | 0 | 2 | 0 | 0 | |
73.16 | 3-20C-6-5,6 | 0 | 5 | 90 | PARTIALLY RECRYSTALLIZED FORAM NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 70 | 5 | 0 | 0 | 0 | 2 | 0 | 2 | |
73.50 | 3-20C-6-5,40 | 0 | 1 | 99 | RECRYSTALLIZED NANNO CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 63 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | |
73.85 | 3-20C-6-5,75 | 0 | 2 | 98 | RECRYSTALLIZED ZEOLITE NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 76 | 2 | 0 | 0 | 0 | 2 | 0 | 2 | |
74.51 | 3-20C-6-51,141 | 0 | 0 | 0 | DOLOMITE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
74.70 | 3-20C-6-CC,0 | 1 | 0 | 100 | RECRYSTALLIZED NANNO CHALK OOZE | Dominat lithology; relative abundance | 0 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 2 |