Hussong, Donald M; Uyeda, Seiya (2005): Smear slide analysis of Hole 60-456A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230884
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
Sharaskin, Anatoly; Packham, G H; Natland, James H; Nakamura, K; Meijer, Arend; Kling, Stanley; Horai, Ki-Iti; Francis, T J G; Ellis, C Howard; Bleil, Ulrich; Blanchet, R; Hussong, Donald M; Uyeda, Seiya (1982): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LX, 929 pp, https://doi.org/10.2973/dsdp.proc.60.1982
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 17.911800 * Longitude: 145.181300
Date/Time Start: 1978-04-12T00:00:00 * Date/Time End: 1978-04-12T00:00:00
Minimum DEPTH, sediment/rock: 3.35 m * Maximum DEPTH, sediment/rock: 114.52 m
Event(s):
60-456A * Latitude: 17.911800 * Longitude: 145.181300 * Date/Time: 1978-04-12T00:00:00 * Elevation: -3586.0 m * Penetration: 159 m * Recovery: 37.5 m * Location: North Pacific/SEDIMENT POND * Campaign: Leg60 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 15 cores; 139.5 m cored; 0 m drilled; 26.9 % 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 | Radiolarians | Rad | % | Smear slide analysis | ||
13 | Diatoms | Diatoms | % | Smear slide analysis | ||
14 | Spiculae | Spiculae | % | Smear slide analysis | ||
15 | Feldspar | Fsp | % | Smear slide analysis | ||
16 | Zeolite | Zeo | % | Smear slide analysis | ||
17 | Clay minerals | Clay min | % | Smear slide analysis | ||
18 | Opaque minerals | Opaque | % | Smear slide analysis | ||
19 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
20 | Iron | Fe | % | Smear slide analysis | ||
21 | Heavy minerals | HM | % | Smear slide analysis | ||
22 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
23 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
24 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1057 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 Rad [%] | 13 Diatoms [%] | 14 Spiculae [%] | 15 Fsp [%] | 16 Zeo [%] | 17 Clay min [%] | 18 Opaque [%] | 19 Py [%] | 20 Fe [%] | 21 HM [%] | 22 Volc glass [%] | 23 Rock fragm [%] | 24 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
3.35 | 60-456A-1-3,35 | 10 | 20 | 70 | Quaternary | MARLY CALCAREOUS OOZE | Dominat lithology; relative abundance | 0 | 50 | 10 | 1 | 0 | 0 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
5.60 | 60-456A-1-41,110 | 3 | 75 | 22 | Quaternary | MARLY SILICEOUS FORAM OOZE | numerical abundance | 2 | 15 | 20 | 10 | 20 | 1 | 10 | 0 | 1 | 0 | 0 | 1 | 1 | 18 | 0 | 1 |
5.61 | 60-456A-1-41,111 | 5 | 45 | 50 | Quaternary | VITRIC MUD WITH NANNOS AND DIATOMS | Dominat lithology; numerical abundance | 0 | 30 | 0 | 5 | 15 | 0 | 5 | 0 | 20 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
5.68 | 60-456A-1-41,118 | 60 | 30 | 10 | Quaternary | SANDY VITRIC ASH | Minor lithology; numerical abundance | 0 | 5 | 0 | 0 | 0 | 0 | 35 | 0 | 10 | 0 | 0 | 0 | 0 | 50 | 0 | 0 |
7.30 | 60-456A-1-51,130 | 10 | 65 | 25 | Quaternary | SILTY CRYSTAL VITRIC ASH | relative abundance | 2 | 2 | 2 | 1 | 0 | 1 | 10 | 0 | 22 | 0 | 0 | 0 | 1 | 60 | 0 | 1 |
8.00 | 60-456A-1-6,50 | 60 | 39 | 1 | Quaternary | SANDY CRYSTAL VITRIC ASH | numerical abundance | 0 | 0 | 1 | 0 | 0 | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 5 | 60 | 4 | 0 |
38.50 | 60-456A-3-1,50 | 4 | 80 | 16 | Quaternary | SILTY CRYSTAL VITRIC ASH | numerical abundance | 0 | 0 | 0 | 1 | 2 | 0 | 25 | 0 | 9 | 0 | 0 | 0 | 3 | 50 | 10 | 0 |
38.57 | 60-456A-3-1,57 | 10 | 50 | 40 | Quaternary | SILTY VITRIC MUD | Minor lithology; numerical abundance | 0 | 10 | 0 | 2 | 0 | 0 | 25 | 0 | 28 | 0 | 0 | 0 | 0 | 35 | 0 | 0 |
39.00 | 60-456A-3-11,100 | 5 | 65 | 30 | Quaternary | SILTY CRYSTAL VITRIC ASH | numerical abundance | 0 | 0 | 0 | 1 | 0 | 0 | 25 | 0 | 27 | 10 | 0 | 0 | 2 | 40 | 0 | 0 |
40.02 | 60-456A-3-2,52 | 5 | 65 | 30 | Quaternary | SILTY VITRIC ASH | Dominat lithology; numerical abundance | 0 | 10 | 0 | 5 | 0 | 0 | 25 | 0 | 20 | 0 | 0 | 0 | 0 | 40 | 0 | 0 |
40.49 | 60-456A-3-2,99 | 70 | 25 | 5 | Quaternary | SANDY CRYSTAL VITRIC ASH | relative abundance | 0 | 0 | 0 | 0 | 1 | 2 | 15 | 0 | 0 | 0 | 0 | 0 | 4 | 40 | 40 | 0 |
40.55 | 60-456A-3-21,105 | 1 | 79 | 20 | Quaternary | SILTY CRYSTAL VITRIC ASH | numerical abundance | 2 | 3 | 3 | 0 | 3 | 1 | 15 | 0 | 5 | 0 | 0 | 0 | 3 | 65 | 0 | 0 |
40.85 | 60-456A-3-21,135 | 2 | 73 | 25 | Quaternary | SILTY CRYSTAL VITRIC ASH | numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 22 | 0 | 0 | 0 | 1 | 60 | 5 | 1 |
41.35 | 60-456A-3-3,35 | 5 | 20 | 75 | Quaternary | VITRIC MUD | numerical abundance | 0 | 10 | 0 | 0 | 0 | 0 | 10 | 0 | 60 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
48.12 | 60-456A-4-CC,4 | 0 | 35 | 65 | Upper pleistocene | VITRIC MARLY NANNO OOZE | numerical abundance | 0 | 30 | 0 | 0 | 0 | 0 | 10 | 0 | 35 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
57.70 | 60-456A-5-1,70 | 2 | 78 | 20 | Lower pleistocene | SILTY VITRIC TUFF (ZEOLITIZED) | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 10 | 18 | 0 | 0 | 1 | 1 | 50 | 0 | 0 |
57.73 | 60-456A-5-1,73 | 0 | 30 | 70 | Lower pleistocene | VITRIC NANNOFOSSIL OOZE | Minor lithology; numerical abundance | 10 | 60 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 0 | 0 |
57.90 | 60-456A-5-1,90 | 0 | 90 | 10 | Lower pleistocene | ACIDIC SILTY VITRIC TUFF | numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 94 | 0 | 1 |
58.09 | 60-456A-5-11,109 | 10 | 60 | 30 | Lower pleistocene | ZEOLITIC CRYSTAL VITRIC TUFF | relative abundance | 1 | 1 | 0 | 0 | 0 | 1 | 15 | 10 | 25 | 0 | 0 | 2 | 2 | 50 | 0 | 0 |
58.25 | 60-456A-5-11,125 | 8 | 57 | 35 | Lower pleistocene | SILTY VITRIC TUFF | numerical abundance | 1 | 0 | 0 | 0 | 0 | 0 | 10 | 1 | 25 | 0 | 0 | 0 | 2 | 60 | 0 | 1 |
58.62 | 60-456A-5-2,12 | 30 | 30 | 30 | Lower pleistocene | SILTY VITRIC TUFF | Dominat lithology; relative abundance | 0 | 20 | 0 | 0 | 0 | 0 | 20 | 1 | 10 | 0 | 0 | 0 | 0 | 40 | 0 | 0 |
58.89 | 60-456A-5-2,39 | 3 | 40 | 57 | Lower pleistocene | SILTY VITRIC TUFF | Minor lithology; relative abundance | 1 | 10 | 0 | 0 | 0 | 0 | 10 | 1 | 40 | 0 | 0 | 0 | 0 | 40 | 0 | 0 |
59.08 | 60-456A-5-2,58 | 0 | 30 | 70 | Lower pleistocene | VITRIC NANNO OOZE | Dominat lithology; numerical abundance | 10 | 60 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
66.79 | 60-456A-6-1,29 | 0 | 20 | 80 | Lower pleistocene | VITRIC NANNO CHALK | relative abundance | 0 | 60 | 0 | 0 | 0 | 0 | 1 | 1 | 20 | 0 | 0 | 0 | 0 | 20 | 0 | 0 |
67.08 | 60-456A-6-1,58 | 10 | 30 | 60 | Lower pleistocene | VITRIC NANNO CHALK | Minor lithology; numerical abundance | 0 | 30 | 0 | 0 | 0 | 0 | 10 | 0 | 30 | 0 | 0 | 0 | 0 | 30 | 0 | 0 |
68.62 | 60-456A-6-2,62 | 15 | 45 | 40 | Lower pleistocene | ZEOLITIZED CRYSTAL VITRIC TUFF | Minor lithology; numerical abundance | 3 | 0 | 0 | 0 | 0 | 0 | 25 | 15 | 13 | 1 | 0 | 0 | 3 | 40 | 0 | 0 |
69.40 | 60-456A-6-21,140 | 5 | 55 | 40 | Lower pleistocene | CRYSTAL MUDSTONE | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 38 | 2 | 34 | 2 | 0 | 1 | 3 | 15 | 0 | 5 |
76.23 | 60-456A-7-1,23 | 0 | 10 | 90 | Lower pleistocene | NANNO CHALK | relative abundance | 10 | 60 | 0 | 0 | 0 | 0 | 1 | 5 | 20 | 0 | 0 | 0 | 0 | 5 | 0 | 0 |
76.99 | 60-456A-7-1,99 | 10 | 30 | 60 | Lower pleistocene | MUDDY VITRIC TUFF | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 15 | 0 | 0 | 0 | 0 | 82 | 0 | 0 |
77.90 | 60-456A-7-2,40 | 20 | 60 | 20 | Lower pleistocene | SILTY VITRIC TUFF | relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 4 | 0 | 0 | 0 | 1 | 90 | 0 | 0 |
85.90 | 60-456A-8-1,40 | 60 | 25 | 15 | Lower pleistocene | SANDY VITRIC TUFF | numerical abundance | 1 | 1 | 0 | 0 | 0 | 0 | 15 | 0 | 12 | 0 | 0 | 0 | 2 | 50 | 0 | 0 |
87.25 | 60-456A-8-2,25 | 10 | 50 | 40 | Lower pleistocene | SILTY CRYSTAL VITRIC TUFF | numerical abundance | 1 | 1 | 0 | 0 | 0 | 0 | 15 | 1 | 39 | 0 | 0 | 0 | 3 | 40 | 0 | 0 |
87.57 | 60-456A-8-2,57 | 50 | 20 | 30 | Lower pleistocene | SANDY VITRIC TUFF (WITH CHLORITE) | numerical abundance | 10 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 20 | 0 | 0 | 0 | 0 | 60 | 0 | 0 |
87.58 | 60-456A-8-2,58 | 2 | 8 | 90 | Lower pleistocene | VITRIC MARLY CHALK | numerical abundance | 10 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 | 0 | 0 | 0 | 10 | 0 | 0 |
87.60 | 60-456A-8-2,60 | 0 | 5 | 95 | Lower pleistocene | CALCAREOUS MUDSTONE | numerical abundance | 10 | 10 | 0 | 0 | 0 | 0 | 5 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
95.70 | 60-456A-9-1,70 | 40 | 50 | 10 | Lower pleistocene | SANDY VITRIC TUFF | numerical abundance | 4 | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 10 | 3 | 0 | 0 | 5 | 70 | 0 | 0 |
96.56 | 60-456A-9-2,6 | 80 | 20 | 0 | Lower pleistocene | CHLORITIZED SANDY VITRIC TUFF | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 |
96.67 | 60-456A-9-2,17 | 10 | 20 | 70 | Lower pleistocene | MUDDY VITRIC TUFF | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 95 | 0 | 0 |
97.58 | 60-456A-9-21,108 | 40 | 40 | 20 | Lower pleistocene | SILTY VITRIC TUFF | numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 98 | 0 | 0 |
98.10 | 60-456A-9-3,10 | 50 | 25 | 25 | Lower pleistocene | ZEOLITIZED SANDY VITRIC TUFF | numerical abundance | 3 | 0 | 0 | 0 | 0 | 0 | 10 | 15 | 20 | 0 | 0 | 0 | 2 | 50 | 0 | 0 |
105.51 | 60-456A-10-11,101 | 5 | 55 | 40 | Lower pleistocene | CLAYSTONE (OR CHLORITISED SILTY TUFF) | numerical abundance | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 3 | 82 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
105.52 | 60-456A-10-11,102 | 5 | 30 | 65 | Lower pleistocene | CALCAREOUS MUDSTONE | numerical abundance | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 53 | 0 | 0 | 0 | 0 | 0 | 0 | 15 |
108.22 | 60-456A-10-3,72 | 0 | 20 | 80 | Lower pleistocene | CALCAREOUS MUDSTONE WITH PYRITE | numerical abundance | 15 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 81 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
108.24 | 60-456A-10-3,74 | 0 | 10 | 90 | Lower pleistocene | MARLY CHALK WITH PYRITE | numerical abundance | 43 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 50 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
109.22 | 60-456A-10-4,22 | 1 | 49 | 50 | Lower pleistocene | ALTERED MUDSTONE | numerical abundance | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 87 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
114.52 | 60-456A-11-1,2 | 0 | 35 | 65 | CALCAREOUS MUDSTONE | numerical abundance | 25 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 65 | 5 | 0 | 0 | 0 | 5 | 0 | 0 |