Laughton, Anthony S; Berggren, William A (2005): Smear slide analysis of Hole 12-116A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230342
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
Whitmarsh, Robert B; van Hinte, Jan E; Ruffman, A; Perch-Nielsen, Katharina; Musich, L F; Franz, Ulrich; Davies, Thomas A; Benson, Richard N; Laughton, Anthony S; Berggren, William A (1972): Initial Reports of the Deep Sea Drilling Project 12. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, XII, 1243 pp, https://doi.org/10.2973/dsdp.proc.12.1972
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 57.496000 * Longitude: -15.924300
Date/Time Start: 1970-07-17T00:00:00 * Date/Time End: 1970-07-17T00:00:00
Minimum DEPTH, sediment/rock: 0.95 m * Maximum DEPTH, sediment/rock: 98.53 m
Event(s):
12-116A * Latitude: 57.496000 * Longitude: -15.924300 * Date/Time: 1970-07-17T00:00:00 * Elevation: -1151.0 m * Penetration: 99 m * Recovery: 81.7 m * Location: North Atlantic/BASIN * Campaign: Leg12 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 99 m cored; 0 m drilled; 82.5 % 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 | Carbonates | Carb | % | Smear slide analysis | ||
10 | Nannofossils | Nannos | % | Smear slide analysis | ||
11 | Foraminifera | Foram | % | Smear slide analysis | ||
12 | Chalcedony | Chalcedony | % | Smear slide analysis | ||
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Zeolite | Zeo | % | Smear slide analysis | ||
17 | Clay minerals | Clay min | % | Smear slide analysis | ||
18 | Glauconite | Glt | % | Smear slide analysis | ||
19 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
20 | Limonite | Lm | % | Smear slide analysis | ||
21 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
22 | Palagonite | Palagonite | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
882 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 Nannos [%] | 11 Foram [%] | 12 Chalcedony [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Spiculae [%] | 16 Zeo [%] | 17 Clay min [%] | 18 Glt [%] | 19 Py [%] | 20 Lm [%] | 21 Volc glass [%] | 22 Palagonite [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.95 | 12-116A-1-1,95 | 60 | 60 | 0 | Pleistocene | FORAM RICH SANDY SILT | Dominat lithology; numerical abundance | 0 | 14 | 33 | 0 | 0 | 14 | 14 | 4 | 0 | 0 | 4 | 0 | 14 | 4 |
1.63 | 12-116A-1-2,13 | 35 | 60 | 35 | Pleistocene | SANDY CLAYEY SILT | Minor lithology; numerical abundance | 14 | 14 | 14 | 0 | 0 | 4 | 14 | 0 | 0 | 0 | 4 | 0 | 33 | 4 |
1.70 | 12-116A-1-2,20 | 35 | 35 | 0 | Pleistocene | SANDY SILT | Dominat lithology; numerical abundance | 15 | 15 | 15 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 4 | 4 | 37 | 4 |
3.10 | 12-116A-1-CC,0 | 35 | 35 | 10 | Pleistocene | SILTY SANDY MARL | Dominat lithology; relative abundance | 23 | 23 | 23 | 0 | 0 | 6 | 6 | 6 | 0 | 6 | 6 | 0 | 23 | 6 |
10.20 | 12-116A-2-11,120 | 0 | 0 | 0 | Pleistocene | FORAM OOZE | Dominat lithology; numerical abundance | 4 | 15 | 50 | 0 | 0 | 4 | 15 | 0 | 0 | 0 | 4 | 0 | 4 | 4 |
12.60 | 12-116A-2-3,60 | 60 | 35 | 10 | Pleistocene | SANDY SILTY MARL | Dominat lithology; numerical abundance | 4 | 14 | 35 | 0 | 0 | 14 | 14 | 0 | 0 | 0 | 14 | 0 | 0 | 4 |
13.90 | 12-116A-2-4,40 | 35 | 60 | 10 | Pleistocene | SANDY SILTY MARL | Dominat lithology; numerical abundance | 16 | 39 | 16 | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 16 | 4 |
15.80 | 12-116A-2-5,80 | 60 | 35 | 10 | Pleistocene | SANDY SILTY MARL | Dominat lithology; relative abundance | 6 | 23 | 55 | 0 | 0 | 6 | 0 | 6 | 0 | 6 | 6 | 0 | 23 | 6 |
16.60 | 12-116A-2-CC,0 | 60 | 35 | 10 | Pleistocene | SANDY SILTY MARL | Dominat lithology; numerical abundance | 4 | 15 | 36 | 0 | 0 | 15 | 4 | 4 | 0 | 0 | 4 | 0 | 15 | 4 |
19.02 | 12-116A-3-11,102 | 35 | 60 | 10 | Pleistocene | SANDY SILT | Minor lithology; relative abundance | 23 | 23 | 6 | 0 | 0 | 0 | 0 | 6 | 23 | 0 | 6 | 0 | 23 | 6 |
20.25 | 12-116A-3-2,75 | 35 | 35 | 10 | Pleistocene | SANDY SILT | Dominat lithology; numerical abundance | 12 | 12 | 12 | 0 | 0 | 3 | 3 | 12 | 0 | 0 | 3 | 0 | 29 | 12 |
20.70 | 12-116A-3-21,120 | 35 | 85 | 10 | Pleistocene | FORAM NANNO OOZE | Minor lithology; numerical abundance | 13 | 42 | 13 | 0 | 0 | 13 | 3 | 0 | 0 | 0 | 3 | 0 | 13 | 0 |
24.75 | 12-116A-3-5,75 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 24 | 24 | 0 | 0 | 10 | 24 | 0 | 0 | 0 | 3 | 0 | 3 | 3 |
26.25 | 12-116A-3-6,75 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 22 | 22 | 0 | 0 | 10 | 22 | 0 | 0 | 0 | 3 | 0 | 10 | 0 |
26.90 | 12-116A-3-61,140 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 11 | 27 | 27 | 0 | 3 | 11 | 3 | 0 | 0 | 0 | 3 | 0 | 11 | 3 |
27.10 | 12-116A-3-CC,0 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 3 | 31 | 42 | 0 | 0 | 3 | 13 | 0 | 0 | 0 | 3 | 0 | 3 | 0 |
28.20 | 12-116A-4-11,120 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 14 | 35 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 4 | 4 | 4 |
30.60 | 12-116A-4-3,60 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 3 | 27 | 27 | 3 | 3 | 11 | 11 | 0 | 0 | 0 | 3 | 0 | 11 | 0 |
31.85 | 12-116A-4-4,35 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 13 | 31 | 13 | 0 | 3 | 13 | 13 | 0 | 0 | 0 | 0 | 0 | 13 | 0 |
32.65 | 12-116A-4-41,115 | 0 | 0 | 0 | Pleistocene | NANNO OOZE | Minor lithology; numerical abundance | 36 | 36 | 4 | 0 | 0 | 4 | 4 | 4 | 0 | 0 | 0 | 4 | 4 | 4 |
34.00 | 12-116A-4-51,100 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 25 | 25 | 0 | 0 | 10 | 10 | 0 | 0 | 0 | 3 | 3 | 10 | 3 |
35.25 | 12-116A-4-6,75 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 3 | 28 | 28 | 0 | 0 | 12 | 12 | 0 | 0 | 0 | 0 | 3 | 12 | 3 |
38.28 | 12-116A-5-2,78 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 2 | 22 | 22 | 0 | 0 | 9 | 22 | 0 | 0 | 0 | 0 | 0 | 22 | 2 |
39.75 | 12-116A-5-3,75 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 10 | 23 | 32 | 0 | 0 | 10 | 10 | 0 | 0 | 0 | 3 | 0 | 10 | 3 |
48.75 | 12-116A-6-3,75 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 13 | 31 | 13 | 0 | 0 | 13 | 13 | 0 | 0 | 0 | 3 | 0 | 13 | 0 |
51.75 | 12-116A-6-5,75 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 11 | 26 | 26 | 0 | 0 | 11 | 11 | 0 | 0 | 0 | 0 | 0 | 11 | 4 |
53.30 | 12-116A-6-6,80 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 12 | 29 | 12 | 0 | 0 | 3 | 12 | 0 | 0 | 0 | 3 | 3 | 12 | 12 |
53.35 | 12-116A-6-6,85 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 12 | 29 | 29 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 3 | 0 | 12 | 3 |
53.85 | 12-116A-6-61,135 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 6 | 75 | 23 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 6 | 6 | 6 | 0 |
55.08 | 12-116A-7-11,108 | 0 | 0 | 0 | Pleistocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 12 | 29 | 29 | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 12 | 12 |
62.52 | 12-116A-7-61,102 | 0 | 0 | 0 | Pliocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 23 | 0 | 23 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 6 | 0 | 23 | 6 |
62.55 | 12-116A-7-61,105 | 0 | 0 | 0 | Pliocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 0 | 36 | 15 | 0 | 4 | 15 | 15 | 0 | 0 | 0 | 0 | 0 | 15 | 0 |
71.25 | 12-116A-8-6,75 | 0 | 0 | 0 | Pliocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 3 | 31 | 31 | 0 | 3 | 13 | 13 | 0 | 0 | 0 | 3 | 0 | 3 | 0 |
80.25 | 12-116A-9-6,75 | 0 | 0 | 0 | Pliocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 3 | 31 | 31 | 0 | 0 | 13 | 13 | 0 | 0 | 0 | 3 | 0 | 3 | 3 |
81.10 | 12-116A-9-CC,0 | 0 | 0 | 0 | Pliocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 6 | 75 | 23 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
82.07 | 12-116A-10-11,107 | 0 | 0 | 0 | Pliocene | NANNO FORAM OOZE | Dominat lithology; numerical abundance | 13 | 42 | 3 | 0 | 0 | 3 | 13 | 0 | 0 | 0 | 13 | 0 | 13 | 0 |
82.20 | 12-116A-10-11,120 | 0 | 0 | 0 | Pliocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 6 | 75 | 6 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
92.53 | 12-116A-11-2,75 | 0 | 0 | 0 | Pliocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 4 | 36 | 15 | 0 | 0 | 4 | 15 | 15 | 0 | 0 | 4 | 0 | 4 | 4 |
94.03 | 12-116A-11-3,75 | 0 | 0 | 0 | Pliocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 6 | 75 | 23 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
95.53 | 12-116A-11-4,75 | 0 | 0 | 0 | Pliocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 4 | 33 | 14 | 0 | 0 | 14 | 14 | 4 | 0 | 0 | 0 | 0 | 14 | 4 |
97.03 | 12-116A-11-5,75 | 35 | 60 | 10 | Pliocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 4 | 32 | 13 | 0 | 0 | 13 | 13 | 4 | 0 | 0 | 4 | 0 | 13 | 4 |
98.53 | 12-116A-11-6,75 | 60 | 60 | 10 | Pliocene | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 3 | 25 | 25 | 0 | 0 | 10 | 10 | 10 | 0 | 0 | 3 | 0 | 10 | 3 |