Bader, Richard G; Gerard, Robert D (2005): Smear slide analysis of Hole 4-28 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230688
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
Sayles, Frederick L; Riedel, William R; Ruef, Michael H; Rothwell, W Thomas; Hay, William W; Bolli, Hans M; Benson, William E; Gerard, Robert D; Bader, Richard G (1970): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, IV, 751 pp, https://doi.org/10.2973/dsdp.proc.4.1970
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 20.586500 * Longitude: -65.622200
Date/Time Start: 1969-03-03T00:00:00 * Date/Time End: 1969-03-03T00:00:00
Minimum DEPTH, sediment/rock: 69.64 m * Maximum DEPTH, sediment/rock: 399.10 m
Event(s):
4-28 * Latitude: 20.586500 * Longitude: -65.622200 * Date/Time: 1969-03-03T00:00:00 * Elevation: -5251.0 m * Penetration: 404 m * Recovery: 13 m * Location: North Atlantic/RIDGE * Campaign: Leg4 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 5 cores; 74 m cored; 36 m drilled; 17.6 % 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 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Nannofossils | Nannos | % | Smear slide analysis | ||
12 | Foraminifera | Foram | % | Smear slide analysis | ||
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Components indeterminata | Comp indet | % | Smear slide analysis | other fossils | |
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Minerals, other | Min other | % | Smear slide analysis | ||
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Mica | Mica | % | Smear slide analysis | ||
22 | Clay minerals | Clay min | % | Smear slide analysis | ||
23 | Opaque minerals | Opaque | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
26 | Pumice | Pumice | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1347 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 Rad [%] | 14 Diatoms [%] | 15 Comp indet [%] | 16 Spiculae [%] | 17 Min other [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Mica [%] | 22 Clay min [%] | 23 Opaque [%] | 24 Py [%] | 25 Volc glass [%] | 26 Pumice [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
69.64 | 4-28-2-2,14 | 0 | 10 | 70 | Upper eocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 0 | 0 |
69.85 | 4-28-2-2,35 | 0 | 0 | 0 | Upper eocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | 2 | 95 | 0 | 0 | 0 | 0 |
70.37 | 4-28-2-2,87 | 0 | 10 | 90 | Upper eocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 2 | 0 | 90 | 0 | 0 | 0 | 0 |
70.38 | 4-28-2-2,88 | 0 | 0 | 0 | Upper eocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 20 | 0 | 0 | 70 | 0 | 0 | 5 | 0 |
70.72 | 4-28-2-21,122 | 0 | 70 | 30 | Upper eocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 |
70.77 | 4-28-2-21,127 | 0 | 0 | 0 | Upper eocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 95 | 0 | 0 | 0 | 0 |
70.93 | 4-28-2-21,143 | 0 | 20 | 80 | Upper eocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 80 | 0 | 0 | 0 | 0 |
70.99 | 4-28-2-21,149 | 0 | 30 | 70 | Upper eocene | CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 70 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 |
71.20 | 4-28-2-3,20 | 0 | 0 | 0 | Upper eocene | SLIGHTLY SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 7 | 0 | 0 | 90 | 0 | 0 | 0 | 0 |
71.54 | 4-28-2-3,54 | 0 | 0 | 0 | Upper eocene | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 90 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | |
71.64 | 4-28-2-3,64 | 0 | 0 | 0 | Upper eocene | BLACK MATERIAL | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
72.10 | 4-28-2-31,110 | 0 | 0 | 0 | Upper eocene | SLIGHTLY SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 7 | 0 | 0 | 90 | 0 | 0 | 0 | 0 |
72.70 | 4-28-2-4,20 | 0 | 0 | 0 | Upper eocene | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 3 | 90 | 0 | 0 | 0 | 0 |
73.09 | 4-28-2-4,59 | 0 | 0 | 0 | Upper eocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 40 | 0 | 0 | 0 | 0 |
73.63 | 4-28-2-41,113 | 0 | 0 | 0 | Upper eocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 100 | 0 | 0 | 0 | 0 |
73.90 | 4-28-2-41,140 | 0 | 0 | 0 | Upper eocene | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 70 | 0 | 0 | 0 | 0 | 0 | 0 |
74.10 | 4-28-2-CC,0 | 0 | 0 | 0 | Upper eocene | CLAY | Dominat lithology; numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 3 | 0 | 0 | 0 | 96 | 0 | 0 | 0 | 0 |
169.10 | 4-28-3-0,10 | 0 | 50 | 50 | Upper eocene | CHALKY OOZE (CLAY) | Dominat lithology; numerical abundance | 0 | 0 | 60 | 0 | 10 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
169.26 | 4-28-3-0,26 | 0 | 0 | 0 | Upper eocene | CHALKY OOZE (CLAY) | Dominat lithology; relative abundance | 0 | 0 | 60 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 10 | 25 | 0 | 0 | 0 | 0 |
169.70 | 4-28-3-0,70 | 0 | 70 | 30 | Upper eocene | CHALKY OOZE (CLAY) | Dominat lithology; numerical abundance | 0 | 0 | 50 | 0 | 5 | 20 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
169.97 | 4-28-3-1,20 | 10 | 70 | 20 | Upper eocene | NANNO FORAM DIATOM SPONGE SPICULE OOZE | Dominat lithology; numerical abundance | 0 | 0 | 30 | 20 | 10 | 10 | 0 | 20 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
170.17 | 4-28-3-1,40 | 10 | 50 | 40 | Upper eocene | NANNO FORAM DIATOM SPONGE SPICULE OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 20 | 10 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 |
171.33 | 4-28-3-2,6 | 1 | 60 | 40 | Upper eocene | CLAYEY SILT | Dominat lithology; relative abundance | 0 | 0 | 40 | 2 | 5 | 25 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
172.07 | 4-28-3-2,80 | 5 | 65 | 30 | Upper eocene | CLAYEY SILT | Dominat lithology; relative abundance | 0 | 0 | 40 | 2 | 10 | 20 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
173.07 | 4-28-3-3,30 | 5 | 75 | 20 | Upper eocene | CLAYEY SILT | Dominat lithology; relative abundance | 0 | 0 | 50 | 2 | 10 | 20 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
174.33 | 4-28-3-4,6 | 5 | 60 | 35 | Upper eocene | CALCAREOUS CLAY | Dominat lithology; numerical abundance | 0 | 0 | 40 | 5 | 5 | 20 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
174.73 | 4-28-3-4,46 | 30 | 40 | 30 | Upper eocene | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 50 | 5 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 |
175.47 | 4-28-3-41,120 | 5 | 55 | 40 | Upper eocene | CALCAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 45 | 2 | 10 | 15 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 | 0 |
176.37 | 4-28-3-5,60 | 0 | 65 | 35 | Upper eocene | CLAY | Dominat lithology; relative abundance | 0 | 0 | 50 | 2 | 5 | 20 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
177.60 | 4-28-4-CC,0 | 0 | 0 | 0 | Upper eocene | FORAM NANNO DIATOM OOZE IN CLAY | Dominat lithology; numerical abundance | 10 | 0 | 20 | 10 | 10 | 6 | 5 | 10 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 |
177.60 | 4-28-4-CC,0 | 0 | 0 | 0 | Upper eocene | FOSSILIFEROUS CALCAREOUS CLAY | Dominat lithology; numerical abundance | 15 | 0 | 25 | 5 | 10 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 34 | 0 | 0 | 0 | 0 |
177.60 | 4-28-4-CC,0 | 0 | 0 | 0 | Upper eocene | FOSSILIFEROUS CALCAREOUS CLAY | Dominat lithology; numerical abundance | 20 | 0 | 30 | 5 | 7 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 0 | 0 | 0 |
177.66 | 4-28-3-6,39 | 0 | 70 | 30 | Upper eocene | CALCAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 50 | 2 | 5 | 20 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
178.54 | 4-28-3-61,127 | 0 | 70 | 30 | Middle eocene | CLACAREOUS CLAY | Dominat lithology; relative abundance | 0 | 0 | 45 | 2 | 5 | 30 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 |
236.10 | 4-28-5-CC,0 | 0 | 0 | 0 | Middle eocene | CLAY | Dominat lithology; numerical abundance | 50 | 6 | 10 | 10 | 2 | 0 | 0 | 0 | 5 | 5 | 0 | 50 | 0 | 30 | 0 | 0 | 0 | 0 |
236.10 | 4-28-5-CC,0 | 0 | 0 | 0 | Middle eocene | HIGHLY CALCAREOUS CLAY | Dominat lithology; numerical abundance | 0 | 0 | 10 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 |
236.10 | 4-28-5-CC,0 | 0 | 0 | 0 | Middle eocene | HIGHLY CALCAREOUS SILTY CLAYEY CHALK | Minor lithology; numerical abundance | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 |
236.10 | 4-28-5-CC,0 | 0 | 0 | 0 | Middle eocene | ZEOLITE CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 91 | 0 | 0 | 0 | 0 |
280.60 | 4-28-7-CC,0 | 0 | 0 | 0 | Middle eocene | NANNO CHALKY CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 50 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 48 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | CHALK | Dominat lithology; numerical abundance | 1 | 6 | 10 | 1 | 10 | 0 | 2 | 0 | 0 | 5 | 0 | 0 | 10 | 100 | 20 | 0 | 0 | 30 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | CLAYSTONE | Dominat lithology; numerical abundance | 1 | 0 | 10 | 10 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 17 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | CLAYSTONE | Dominat lithology; numerical abundance | 16 | 0 | 19 | 2 | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | CLAYSTONE | Dominat lithology; numerical abundance | 40 | 0 | 2 | 5 | 40 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 35 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 20 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 45 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | NANNO CARBONATE CHALK OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 58 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | NANNO FORAM CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | NANNO FORAM OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 63 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | RAD NANNO CHALK | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 80 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | RADIOLARIAN BENTONITIC ARGILLITE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 84 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | RADIOLARIAN CLAYSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 87 | 0 | 0 | 0 | 0 |
345.10 | 4-28-8-CC,0 | 0 | 0 | 0 | Middle eocene | RADIOLARIAN SILICEOUS CLAYSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 97 | 0 | 0 | 0 | 0 |
399.10 | 4-28-9-CC,0 | 0 | 0 | 0 | CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 15 | 23 | 76 | 0 | 5 | 0 | 0 | |
399.10 | 4-28-9-CC,0 | 0 | 0 | 0 | SILTY CLAY | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 | 0 | 0 |