Thiede, Jörn; Vallier, Tracy L (2005): Smear slide analysis of Hole 62-466 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230899
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
Vincent, Edith; Windom, Kenneth E; Schmidt, Ronald R; Schaaf, André; Seifert, Karl E; Sayre, W O; Sancetta, Constance A; Rea, David K; Koporulin, V I; Fujii, Naoyuki; Dean, Walter E; Cepek, Pavel; Boersma, Anne; Adelseck, C; Thiede, Jörn; Vallier, Tracy L (1981): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXII, 1120 pp, https://doi.org/10.2973/dsdp.proc.62.1981
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 34.191000 * Longitude: 179.255700
Date/Time Start: 1978-08-28T00:00:00 * Date/Time End: 1978-08-28T00:00:00
Minimum DEPTH, sediment/rock: 0.20 m * Maximum DEPTH, sediment/rock: 302.80 m
Event(s):
62-466 * Latitude: 34.191000 * Longitude: 179.255700 * Date/Time: 1978-08-28T00:00:00 * Elevation: -2665.0 m * Penetration: 312 m * Recovery: 105.1 m * Location: North Pacific/CONT RISE * Campaign: Leg62 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 33 cores; 302.5 m cored; 9.5 m drilled; 34.7 % 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 | Pteropoda | Pteropoda | % | 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 | Clay minerals | Clay min | % | Smear slide analysis | ||
21 | Glauconite | Glt | % | Smear slide analysis | ||
22 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
23 | Iron | Fe | % | Smear slide analysis | ||
24 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
25 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1412 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 Pteropoda [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Clay min [%] | 21 Glt [%] | 22 Py [%] | 23 Fe [%] | 24 Volc glass [%] | 25 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.20 | 62-466-1-1,20 | 0 | 0 | 0 | Upper pleistocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 5 | 72 | 20 | 0 | 2 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
0.59 | 62-466-1-1,59 | 0 | 0 | 0 | Upper pleistocene | NANNO OOZE | Minor lithology; relative abundance | 8 | 81 | 5 | 0 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
1.00 | 62-466-1-11,100 | 0 | 0 | 0 | Upper pleistocene | RAD NANNO OOZE | Dominat lithology; relative abundance | 8 | 76 | 5 | 0 | 10 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
2.23 | 62-466-1-2,73 | 0 | 0 | 0 | Upper pleistocene | SILICEOUS NANNO OOZE (WHITISH GRAY) | Dominat lithology; relative abundance | 2 | 75 | 10 | 0 | 6 | 5 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
2.80 | 62-466-1-21,130 | 0 | 0 | 0 | Upper pleistocene | RAD NANNO OOZE (GREENISH GRAY) | Dominat lithology; relative abundance | 2 | 70 | 12 | 2 | 7 | 7 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 |
3.74 | 62-466-1-3,74 | 0 | 0 | 0 | Upper pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 10 | 80 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
4.49 | 62-466-1-31,149 | 0 | 0 | 0 | Upper pleistocene | Minor lithology; relative abundance | 5 | 85 | 7 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | |
5.30 | 62-466-1-4,80 | 0 | 0 | 0 | Upper pleistocene | FORAM NANNO OOZE (BROWN) | Dominat lithology; relative abundance | 0 | 79 | 15 | 0 | 3 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.42 | 62-466-1-5,42 | 0 | 0 | 0 | Upper pleistocene | NANNO OOZE (GREEN CLOT) | Minor lithology; numerical abundance | 10 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
8.17 | 62-466-1-CC,0 | 0 | 0 | 0 | Upper pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 1 | 98 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
8.57 | 62-466-2-1,57 | 0 | 0 | 0 | Upper pleistocene | PYRITE BEARING NANNO OOZE | Minor lithology; relative abundance | 0 | 80 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 0 | 0 |
8.70 | 62-466-2-1,70 | 0 | 0 | 0 | Upper pleistocene | GREENISH | Dominat lithology; relative abundance | 5 | 88 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 |
9.35 | 62-466-2-11,135 | 0 | 0 | 0 | Lower pleistocene | NANNO OOZE (WHITE-GRAY) | Dominat lithology; numerical abundance | 5 | 82 | 3 | 0 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
11.08 | 62-466-2-3,8 | 0 | 0 | 0 | Lower pleistocene | NANNO OOZE (WHITE) | Dominat lithology; numerical abundance | 10 | 82 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
15.25 | 62-466-2-51,125 | 0 | 0 | 0 | Lower pleistocene | NANNO OOZE (GREENISH GRAY) | Dominat lithology; numerical abundance | 10 | 78 | 7 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
17.20 | 62-466-2-7,20 | 0 | 0 | 0 | Lower pleistocene | NANNO OOZE | Dominat lithology; numerical abundance | 7 | 82 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
17.75 | 62-466-3-1,25 | 0 | 0 | 0 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 5 | 83 | 6 | 0 | 3 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
20.95 | 62-466-3-3,45 | 0 | 0 | 0 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 5 | 89 | 3 | 0 | 1 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
25.25 | 62-466-3-6,25 | 0 | 0 | 0 | Upper pliocene | NANNO OOZE | Dominat lithology; relative abundance | 4 | 91 | 4 | 0 | 1 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 2 | 0 |
28.10 | 62-466-4-11,110 | 0 | 0 | 0 | Upper pliocene | FORAM NANNO OOZE (GREENISH) | Minor lithology; relative abundance | 0 | 72 | 30 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
28.51 | 62-466-4-2,1 | 0 | 0 | 0 | Upper pliocene | NANNO OOZE (WHITE) | Dominat lithology; relative abundance | 0 | 93 | 5 | 0 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
30.35 | 62-466-4-CC,0 | 0 | 0 | 0 | Upper pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 3 | 85 | 7 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
39.37 | 62-466-5-21,137 | 0 | 0 | 0 | Lower pliocene | NANNO OOZE (WHITE) | Dominat lithology; numerical abundance | 3 | 94 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
41.86 | 62-466-5-4,86 | 0 | 0 | 0 | Lower pliocene | GREEN | Dominat lithology; relative abundance | 3 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
47.37 | 62-466-6-11,137 | 0 | 0 | 0 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 97 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
50.15 | 62-466-6-31,115 | 0 | 0 | 0 | Lower pliocene | NANNO OOZE | Dominat lithology; numerical abundance | 5 | 97 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 |
52.95 | 62-466-6-5,95 | 0 | 0 | 0 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 5 | 95 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
55.38 | 62-466-6-CC,0 | 0 | 0 | 0 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 5 | 90 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
56.05 | 62-466-7-1,55 | 0 | 0 | 0 | Lower pliocene | NANNO OOZE | Minor lithology; relative abundance | 82 | 10 | 8 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
56.25 | 62-466-7-1,75 | 0 | 0 | 0 | Lower pliocene | NANNO OOZE | Dominat lithology; relative abundance | 77 | 20 | 3 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
60.05 | 62-466-7-4,5 | 0 | 0 | 0 | Lower pliocene | NANNO OOZE | Minor lithology; relative abundance | 40 | 48 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 10 | 0 | 0 | 0 | 2 | 0 |
61.05 | 62-466-7-41,105 | 0 | 0 | 0 | Lower pliocene | Dominat lithology; relative abundance | 18 | 80 | 2 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | |
64.65 | 62-466-7-7,15 | 0 | 0 | 0 | Lower pliocene | Dominat lithology; numerical abundance | 5 | 92 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
66.20 | 62-466-8-11,120 | 0 | 0 | 0 | Upper eocene | NANNO OOZE | Dominat lithology; numerical abundance | 20 | 78 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
73.80 | 62-466-8-CC,0 | 0 | 0 | 0 | Upper eocene | RECRYSTALLIZED NANNO-OOZE | Dominat lithology; numerical abundance | 48 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
74.64 | 62-466-9-1,14 | 0 | 0 | 0 | Upper eocene | ZEOLITE NANNO OOZE DARK BROWN | Minor lithology; numerical abundance | 30 | 54 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 2 | 0 | 0 | 2 | 2 | 0 |
75.40 | 62-466-9-1,90 | 0 | 0 | 0 | Upper eocene | NANNO OOZE | Dominat lithology; relative abundance | 30 | 64 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 3 | 0 | 0 |
79.55 | 62-466-9-4,55 | 0 | 0 | 0 | Upper eocene | NANNO OOZE | Dominat lithology; numerical abundance | 20 | 75 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
88.45 | 62-466-11-1,45 | 0 | 0 | 0 | Upper senonian | Dominat lithology; numerical abundance | 15 | 82 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
89.25 | 62-466-11-11,125 | 0 | 0 | 0 | Upper senonian | NANNO OOZE | Dominat lithology; numerical abundance | 10 | 80 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
104.70 | 62-466-13-2,20 | 0 | 0 | 0 | Upper campanian | NANNO OOZE (DARK GREY INCLUSIONS) | Minor lithology; numerical abundance | 15 | 77 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 |
105.55 | 62-466-13-21,105 | 0 | 0 | 0 | Upper campanian | NANNO OOZE | Dominat lithology; relative abundance | 20 | 78 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
124.70 | 62-466-15-21,120 | 0 | 0 | 0 | Upper campanian | NANNO OOZE | Dominat lithology; relative abundance | 10 | 80 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
125.22 | 62-466-15-3,22 | 0 | 0 | 0 | Upper campanian | NANNO OOZE (DARK GREY) | Minor lithology; relative abundance | 10 | 65 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 15 | 0 | 0 | 0 |
133.70 | 62-466-16-2,70 | 0 | 0 | 0 | Middle campanian | NANNO OOZE | Dominat lithology; relative abundance | 4 | 90 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
141.75 | 62-466-17-1,75 | 0 | 0 | 0 | Lower santonian | NANNO OOZE | Dominat lithology; numerical abundance | 5 | 85 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
245.70 | 62-466-28-CC,20 | 0 | 0 | 0 | Upper cretaceous | CLAY (ALT. VOLCANIC ASH) BLACK MUD | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 93 | 0 | 3 | 0 | 2 | 2 |
245.75 | 62-466-28-CC,25 | 0 | 0 | 0 | Upper cretaceous | PYRITIC CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 73 | 2 | 20 | 0 | 0 | 0 |
256.15 | 62-466-29-11,115 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED LIMESTONE | Dominat lithology; numerical abundance | 88 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 1 | 0 | 0 | 0 |
256.65 | 62-466-29-2,15 | 0 | 0 | 0 | Upper albian | CLAY NANNO LIMESTONE | Dominat lithology; numerical abundance | 19 | 50 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 1 | 0 | 0 | 0 |
256.85 | 62-466-29-2,35 | 0 | 0 | 0 | Upper albian | CLAYEY NANNO OOZE | Dominat lithology; numerical abundance | 34 | 40 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 20 | 0 | 1 | 0 | 0 | 0 |
257.29 | 62-466-29-CC,20 | 0 | 0 | 0 | Upper albian | NANNO MARLSTONE | Dominat lithology; numerical abundance | 34 | 30 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 25 | 0 | 3 | 0 | 0 | 0 |
264.68 | 62-466-30-1,18 | 0 | 0 | 0 | Upper albian | LIMESTONE | Minor lithology; numerical abundance | 80 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 |
264.95 | 62-466-30-1,45 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED NANNO LIMESTONE | Dominat lithology; relative abundance | 55 | 30 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 |
274.13 | 62-466-31-1,13 | 0 | 0 | 0 | Upper albian | NANNO OOZE | Minor lithology; numerical abundance | 2 | 86 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 2 | 8 |
274.18 | 62-466-31-1,18 | 0 | 0 | 0 | Upper albian | NANNO LIMESTONE | Dominat lithology; relative abundance | 65 | 20 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 0 | 2 | 0 | 1 | 0 |
293.05 | 62-466-34-1,5 | 0 | 0 | 0 | Upper albian | LIMESTONE (GREY) | Minor lithology; relative abundance | 92 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 3 | 0 | 0 | 0 |
293.40 | 62-466-34-1,40 | 0 | 0 | 0 | Upper albian | NANNO CHALK | Dominat lithology; relative abundance | 58 | 40 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 1 |
302.80 | 62-466-35-1,30 | 0 | 0 | 0 | Upper albian | RECRYSTALLIZED NANNO CHALK | Dominat lithology; numerical abundance | 50 | 40 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 0 | 1 | 0 | 0 | 0 |