Aubouin, Jean; von Huene, Roland (2005): Smear slide analysis of Hole 67-496 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230952
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
Westberg, Jean; Thompson, Peter R; Shiki, Tsunemasa; Muzylov, Nikita; Ladd, John W; Hesse, Reinhard; Harrison, William E; Faas, Richard W; Dengo, Carlos A; Curiale, Joseph A; Cowan, Darrel S; Coulbourn, William T; Azéma, Jacques; Aubouin, Jean; von Huene, Roland (1982): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXVII, 799 pp, https://doi.org/10.2973/dsdp.proc.67.1982
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 13.063700 * Longitude: -90.795200
Date/Time Start: 1979-05-30T00:00:00 * Date/Time End: 1979-05-30T00:00:00
Minimum DEPTH, sediment/rock: 0.12 m * Maximum DEPTH, sediment/rock: 379.60 m
Event(s):
67-496 * Latitude: 13.063700 * Longitude: -90.795200 * Date/Time: 1979-05-30T00:00:00 * Elevation: -2049.0 m * Penetration: 378 m * Recovery: 191.9 m * Location: North Pacific/TRENCH * Campaign: Leg67 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 37 cores; 349.5 m cored; 19 m drilled; 54.9 % 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 | Ostracoda | Ostrac | % | Smear slide analysis | ||
13 | Radiolarians | Rad | % | Smear slide analysis | ||
14 | Diatoms | Diatoms | % | Smear slide analysis | ||
15 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
16 | Spiculae | Spiculae | % | Smear slide analysis | ||
17 | Quartz | Qz | % | Smear slide analysis | ||
18 | Feldspar | Fsp | % | Smear slide analysis | ||
19 | Zeolite | Zeo | % | Smear slide analysis | ||
20 | Mica | Mica | % | Smear slide analysis | ||
21 | Clay minerals | Clay min | % | Smear slide analysis | ||
22 | Glauconite | Glt | % | Smear slide analysis | ||
23 | Opaque minerals | Opaque | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Iron | Fe | % | Smear slide analysis | ||
26 | Heavy minerals | HM | % | Smear slide analysis | ||
27 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
28 | Palagonite | Palagonite | % | Smear slide analysis | ||
29 | Organic matter | OM | % | Smear slide analysis | organic debris | |
30 | Fecal pellets | Fecal pel | % | Smear slide analysis | ||
31 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals | |
32 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1608 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 Ostrac [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Mica [%] | 21 Clay min [%] | 22 Glt [%] | 23 Opaque [%] | 24 Py [%] | 25 Fe [%] | 26 HM [%] | 27 Volc glass [%] | 28 Palagonite [%] | 29 OM [%] | 30 Fecal pel [%] | 31 Minerals [%] | 32 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.12 | 67-496-1-1,12 | 10 | 22 | 68 | Quaternary | DIATOMACEOUS MUD | relative abundance | 0 | 12 | 2 | 0 | 1 | 25 | 1 | 3 | 3 | 1 | 8 | 0 | 31 | 3 | 0 | 2 | 0 | 0 | 8 | 0 | 2 | 0 | 0 | 0 |
6.74 | 67-496-1-5,74 | 5 | 30 | 65 | Quaternary | DIATOMACEOUS MUD | relative abundance | 2 | 10 | 5 | 0 | 2 | 15 | 2 | 1 | 1 | 1 | 10 | 0 | 25 | 3 | 0 | 2 | 0 | 2 | 15 | 0 | 3 | 0 | 0 | 0 |
8.75 | 67-496-2-11,125 | 6 | 29 | 65 | Quaternary | DIATOMACEOUS MUD | relative abundance | 0 | 6 | 1 | 0 | 2 | 36 | 1 | 3 | 3 | 1 | 2 | 0 | 30 | 2 | 0 | 3 | 0 | 0 | 12 | 0 | 2 | 0 | 0 | 0 |
13.87 | 67-496-2-5,37 | 40 | 30 | 30 | Quaternary | CRYSTAL ASH | numerical abundance | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 15 | 5 | 0 | 30 | 1 | 0 | 5 | 0 | 3 | 5 | 2 | 0 | 0 | 20 | 0 |
14.40 | 67-496-2-5,90 | 10 | 40 | 50 | Quaternary | DIATOMACEOUS SILTY MUD | relative abundance | 0 | 6 | 1 | 0 | 1 | 25 | 2 | 2 | 2 | 2 | 1 | 0 | 30 | 0 | 0 | 5 | 0 | 0 | 25 | 0 | 2 | 0 | 0 | 0 |
14.98 | 67-496-2-CC,6 | 15 | 65 | 20 | Quaternary | VITRIC ASH (WHITE) | numerical abundance | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 1 | 0 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 1 |
21.15 | 67-496-3-31,115 | 50 | 40 | 10 | Quaternary | VITRIC-CRYSTAL ASH | numerical abundance | 5 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 20 | 10 | 0 | 0 | 10 | 1 | 0 | 3 | 1 | 1 | 45 | 1 | 0 | 0 | 0 | 0 |
24.29 | 67-496-3-51,129 | 80 | 15 | 5 | Quaternary | TERRIGENOUS SAND | numerical abundance | 2 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 2 | 0 | 45 | 0 | 0 | 20 | 5 | 0 | 0 | 0 | 0 | 0 |
38.30 | 67-496-5-2,80 | 80 | 14 | 6 | Quaternary | VITRIC ASH | relative abundance | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 1 | 5 | 2 | 0 | 0 | 4 | 0 | 0 | 3 | 0 | 2 | 82 | 0 | 0 | 0 | 0 | 0 |
45.72 | 67-496-5-CC,25 | 5 | 35 | 60 | Quaternary | ORGANIC MATTER RICH MUD | numerical abundance | 0 | 5 | 1 | 0 | 3 | 3 | 2 | 5 | 5 | 5 | 0 | 0 | 45 | 0 | 0 | 5 | 1 | 0 | 15 | 0 | 5 | 0 | 0 | 0 |
47.81 | 67-496-6-2,81 | 5 | 30 | 65 | Quaternary | TUFFACEOUS MUD | numerical abundance | 0 | 2 | 3 | 0 | 2 | 5 | 2 | 3 | 15 | 10 | 10 | 0 | 15 | 3 | 0 | 5 | 1 | 0 | 25 | 2 | 2 | 0 | 0 | 0 |
48.94 | 67-496-6-3,44 | 15 | 55 | 30 | Quaternary | TUFFACEOUS MUD | numerical abundance | 0 | 5 | 5 | 0 | 5 | 5 | 1 | 2 | 5 | 2 | 5 | 0 | 20 | 0 | 0 | 2 | 0 | 0 | 40 | 1 | 2 | 0 | 0 | 0 |
52.64 | 67-496-6-51,114 | 8 | 42 | 50 | Quaternary | DIATOMACEOUS MUD WITH VOLC GLASS | relative abundance | 0 | 1 | 2 | 0 | 0 | 28 | 1 | 2 | 4 | 2 | 1 | 0 | 36 | 1 | 0 | 2 | 0 | 1 | 20 | 0 | 2 | 0 | 0 | 0 |
55.39 | 67-496-7-1,39 | 60 | 30 | 10 | Quaternary | VITRIC ASH | numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 |
65.17 | 67-496-8-1,67 | 10 | 30 | 60 | Quaternary | SILICEOUS MUD | numerical abundance | 2 | 3 | 5 | 0 | 5 | 5 | 2 | 5 | 5 | 3 | 1 | 0 | 50 | 0 | 0 | 4 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 |
76.32 | 67-496-9-2,82 | 75 | 15 | 10 | Quaternary | numerical abundance | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 10 | 5 | 0 | 0 | 10 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
85.96 | 67-496-10-2,96 | 0 | 0 | 0 | Quaternary | numerical abundance | 3 | 5 | 2 | 2 | 3 | 44 | 5 | 5 | 5 | 0 | 0 | 0 | 10 | 10 | 0 | 1 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | |
97.50 | 67-496-11-CC,15 | 37 | 23 | 40 | Quaternary | DIATOMACEOUS MUD | numerical abundance | 8 | 0 | 5 | 0 | 3 | 10 | 1 | 1 | 2 | 0 | 0 | 0 | 40 | 3 | 0 | 2 | 0 | 0 | 25 | 0 | 0 | 0 | 0 | 0 |
105.20 | 67-496-12-21,120 | 30 | 20 | 50 | Quaternary | NANNO-FORAM MUD | relative abundance | 0 | 20 | 35 | 0 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 35 | 6 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 |
111.70 | 67-496-12-7,20 | 5 | 25 | 70 | Quaternary | DIATOMACEOUS MUD | relative abundance | 0 | 12 | 2 | 0 | 2 | 18 | 1 | 3 | 4 | 2 | 0 | 0 | 50 | 1 | 0 | 5 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
113.30 | 67-496-13-11,130 | 6 | 20 | 74 | Quaternary | DIATOMACEOUS-NANNOFOSSIL MUD | relative abundance | 0 | 18 | 5 | 0 | 5 | 6 | 2 | 3 | 3 | 2 | 1 | 0 | 46 | 2 | 0 | 3 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
123.70 | 67-496-14-2,70 | 5 | 25 | 70 | Quaternary | NANNOFOSSIL MUD | numerical abundance | 5 | 40 | 5 | 0 | 3 | 2 | 1 | 2 | 2 | 0 | 0 | 0 | 30 | 2 | 0 | 1 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
136.46 | 67-496-15-4,96 | 10 | 30 | 60 | Quaternary | NANNOFOSSIL MUD | numerical abundance | 0 | 43 | 5 | 0 | 1 | 5 | 0 | 10 | 2 | 0 | 0 | 1 | 22 | 8 | 0 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
141.90 | 67-496-16-11,140 | 8 | 40 | 52 | Quaternary | CALCAREOUS SAND | relative abundance | 20 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 2 | 3 | 2 | 0 | 50 | 1 | 0 | 5 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
150.91 | 67-496-17-1,91 | 10 | 30 | 60 | Quaternary | NANNOFOSSIL MUD | numerical abundance | 10 | 30 | 4 | 0 | 5 | 8 | 0 | 8 | 0 | 1 | 0 | 2 | 20 | 5 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
169.73 | 67-496-19-1,73 | 12 | 24 | 64 | Quaternary | NANNOFOSSIL MUD | numerical abundance | 3 | 31 | 2 | 0 | 1 | 10 | 0 | 5 | 2 | 1 | 5 | 2 | 18 | 7 | 0 | 2 | 0 | 3 | 5 | 0 | 0 | 0 | 0 | 0 |
172.62 | 67-496-19-3,62 | 7 | 43 | 50 | Quaternary | CALCAREOUS MUD | relative abundance | 4 | 20 | 4 | 0 | 1 | 5 | 2 | 2 | 2 | 2 | 1 | 0 | 47 | 2 | 0 | 4 | 0 | 2 | 5 | 0 | 0 | 0 | 0 | 0 |
180.70 | 67-496-20-2,70 | 8 | 22 | 70 | Quaternary | HEMIPELAGIC MUD | relative abundance | 3 | 4 | 0 | 0 | 1 | 5 | 0 | 1 | 1 | 2 | 0 | 0 | 68 | 2 | 0 | 4 | 0 | 1 | 8 | 2 | 0 | 0 | 0 | 0 |
188.76 | 67-496-21-1,76 | 10 | 50 | 40 | Quaternary | NANNOFOSSIL MUD | relative abundance | 3 | 29 | 5 | 0 | 5 | 5 | 2 | 15 | 3 | 0 | 0 | 0 | 22 | 5 | 0 | 2 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 |
199.20 | 67-496-21-8,70 | 5 | 20 | 75 | Quaternary | NANNOFOSSIL MUD | numerical abundance | 0 | 25 | 5 | 0 | 2 | 0 | 2 | 2 | 3 | 2 | 2 | 0 | 45 | 0 | 0 | 1 | 0 | 1 | 5 | 0 | 2 | 3 | 0 | 0 |
199.55 | 67-496-22-2,55 | 5 | 15 | 80 | Quaternary | NANNOFOSSIL MUD | numerical abundance | 0 | 35 | 1 | 0 | 0 | 5 | 2 | 2 | 2 | 0 | 4 | 0 | 40 | 1 | 0 | 3 | 0 | 0 | 0 | 1 | 2 | 2 | 0 | 0 |
220.80 | 67-496-24-31,130 | 20 | 55 | 25 | Quaternary | TUFFACEOUS MUD | numerical abundance | 5 | 2 | 5 | 0 | 3 | 3 | 2 | 2 | 3 | 0 | 5 | 0 | 40 | 0 | 0 | 2 | 0 | 0 | 15 | 0 | 3 | 10 | 0 | 0 |
230.55 | 67-496-25-4,5 | 60 | 25 | 15 | Quaternary | TUFFACEOUS MUD | relative abundance | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 15 | 3 | 0 | 5 | 2 | 25 | 0 | 0 | 25 | 0 | 0 | 0 | 15 | 0 | 0 |
230.84 | 67-496-25-4,34 | 25 | 15 | 60 | Quaternary | SANDY MUD | numerical abundance | 10 | 2 | 3 | 0 | 0 | 0 | 0 | 1 | 2 | 8 | 0 | 0 | 55 | 2 | 0 | 2 | 0 | 3 | 5 | 0 | 2 | 5 | 0 | 0 |
243.08 | 67-496-26-6,8 | 60 | 30 | 10 | Upper pliocene | GLAUCONITIC MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | 0 | 10 | 80 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
247.30 | 67-496-27-2,80 | 20 | 20 | 60 | Lower pliocene | HEMIPELAGIC MUD | relative abundance | 0 | 5 | 0 | 0 | 0 | 15 | 0 | 2 | 12 | 2 | 0 | 2 | 25 | 2 | 0 | 5 | 0 | 2 | 35 | 0 | 0 | 2 | 0 | 0 |
254.50 | 67-496-27-CC,10 | 20 | 25 | 55 | Lower pliocene | HEMIPELAGIC MUD | relative abundance | 2 | 15 | 0 | 0 | 2 | 12 | 1 | 3 | 5 | 1 | 0 | 0 | 50 | 3 | 0 | 3 | 0 | 2 | 6 | 0 | 0 | 0 | 0 | 0 |
257.61 | 67-496-28-3,11 | 5 | 5 | 90 | Miocene | NANNOFOSIL MUD | numerical abundance | 0 | 45 | 2 | 0 | 1 | 2 | 0 | 0 | 1 | 1 | 0 | 0 | 45 | 0 | 0 | 1 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 |
262.21 | 67-496-28-CC,21 | 3 | 7 | 90 | Miocene | CALCAREOUS MUDSTONE | relative abundance | 80 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
265.69 | 67-496-29-2,19 | 30 | 25 | 45 | Miocene | SANDY MUD | relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 10 | 8 | 0 | 0 | 45 | 1 | 0 | 1 | 0 | 20 | 10 | 1 | 0 | 3 | 0 | 0 |
268.89 | 67-496-29-4,39 | 15 | 25 | 50 | Miocene | TUFFACEOUS MUD | numerical abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 2 | 5 | 5 | 0 | 48 | 1 | 0 | 1 | 0 | 2 | 15 | 0 | 0 | 20 | 0 | 0 |
270.87 | 67-496-29-5,87 | 20 | 50 | 30 | Miocene | TUFFACEOUS MUD | numerical abundance | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 5 | 5 | 4 | 0 | 30 | 0 | 0 | 1 | 0 | 3 | 40 | 1 | 0 | 10 | 0 | 0 |
280.41 | 67-496-30-5,91 | 5 | 90 | 5 | Middle miocene | VITRIC ASH | numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 |
280.42 | 67-496-30-5,92 | 80 | 15 | 5 | Middle miocene | TUFFACEOUS MUD | relative abundance | 2 | 0 | 1 | 0 | 2 | 0 | 2 | 1 | 5 | 2 | 0 | 0 | 70 | 1 | 0 | 2 | 0 | 1 | 15 | 0 | 0 | 0 | 0 | 0 |
283.89 | 67-496-31-1,89 | 5 | 25 | 70 | Middle miocene | NANNOFOSSIL MUDSTONE | relative abundance | 2 | 48 | 1 | 0 | 0 | 8 | 1 | 2 | 3 | 2 | 0 | 0 | 18 | 3 | 0 | 2 | 0 | 0 | 12 | 0 | 0 | 1 | 0 | 0 |
308.68 | 67-496-33-5,68 | 20 | 20 | 60 | Lower miocene | NANNOFOSSIL SANDY MUD | relative abundance | 1 | 20 | 1 | 0 | 0 | 2 | 1 | 2 | 8 | 1 | 0 | 0 | 45 | 3 | 0 | 2 | 0 | 2 | 15 | 0 | 0 | 2 | 0 | 0 |
313.32 | 67-496-34-2,32 | 30 | 45 | 25 | Lower miocene | numerical abundance | 3 | 2 | 2 | 0 | 1 | 0 | 0 | 1 | 20 | 3 | 0 | 0 | 30 | 1 | 0 | 2 | 0 | 3 | 5 | 0 | 2 | 25 | 0 | 0 | |
329.98 | 67-496-35-CC,50 | 7 | 30 | 63 | Lower miocene | NANNOFOSSIL MUD | numerical abundance | 1 | 18 | 2 | 0 | 1 | 0 | 1 | 3 | 6 | 1 | 0 | 0 | 46 | 2 | 0 | 3 | 0 | 0 | 14 | 0 | 0 | 1 | 0 | 0 |
333.52 | 67-496-36-3,2 | 85 | 12 | 3 | Lower miocene | VITRIC ASHES | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 2 | 0 | 0 | 0 | 2 | 0 | 1 | 0 | 0 | 90 | 0 | 0 | 0 | 0 | 0 |
350.34 | 67-496-38-1,84 | 15 | 45 | 40 | Lower miocene | BIOGENIC MUDSTONE | numerical abundance | 5 | 3 | 5 | 0 | 3 | 0 | 0 | 2 | 10 | 0 | 15 | 0 | 18 | 5 | 0 | 1 | 0 | 4 | 25 | 0 | 0 | 4 | 0 | 0 |
359.11 | 67-496-39-1,11 | 12 | 34 | 54 | Lower miocene | SANDY MUD | relative abundance | 12 | 2 | 4 | 0 | 1 | 2 | 2 | 2 | 5 | 1 | 1 | 0 | 52 | 5 | 0 | 4 | 0 | 1 | 6 | 0 | 0 | 0 | 0 | 0 |
379.60 | 67-496-40-8,60 | 40 | 20 | 40 | ASHY SANDY MUD | numerical abundance | 3 | 3 | 6 | 0 | 2 | 2 | 0 | 3 | 3 | 4 | 1 | 0 | 37 | 4 | 0 | 2 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 |