Thiede, Jörn; Vallier, Tracy L (2005): Smear slide analysis of Hole 62-465. PANGAEA, https://doi.org/10.1594/PANGAEA.230897
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: 33.820500 * Longitude: 178.919000
Date/Time Start: 1978-08-23T00:00:00 * Date/Time End: 1978-08-23T00:00:00
Minimum DEPTH, sediment/rock: 0.05 m * Maximum DEPTH, sediment/rock: 86.97 m
Event(s):
62-465 * Latitude: 33.820500 * Longitude: 178.919000 * Date/Time: 1978-08-23T00:00:00 * Elevation: -2161.0 m * Penetration: 96 m * Recovery: 44.2 m * Location: North Pacific/CONT RISE * Campaign: Leg62 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 96 m cored; 0 m drilled; 46 % 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 | Siliceous microfossils | Silic foss | % | Smear slide analysis | other siliceous material | |
13 | Opal, biogenic silica | bSiO2 | % | Smear slide analysis | ||
14 | Chert | Chert | % | Smear slide analysis | fragments | |
15 | Radiolarians | Rad | % | Smear slide analysis | ||
16 | Diatoms | Diatoms | % | Smear slide analysis | ||
17 | Spiculae | Spiculae | % | Smear slide analysis | ||
18 | Quartz | Qz | % | Smear slide analysis | ||
19 | Feldspar | Fsp | % | Smear slide analysis | ||
20 | Zeolite | Zeo | % | Smear slide analysis | ||
21 | Clay minerals | Clay min | % | Smear slide analysis | ||
22 | Glauconite | Glt | % | Smear slide analysis | ||
23 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
24 | Iron | Fe | % | Smear slide analysis | ||
25 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
26 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
900 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 Silic foss [%] | 13 bSiO2 [%] | 14 Chert [%] | 15 Rad [%] | 16 Diatoms [%] | 17 Spiculae [%] | 18 Qz [%] | 19 Fsp [%] | 20 Zeo [%] | 21 Clay min [%] | 22 Glt [%] | 23 Py [%] | 24 Fe [%] | 25 Volc glass [%] | 26 Minerals [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.05 | 62-465-1-1,5 | 50 | 30 | 20 | Pleistocene | NANNO FORAM OOZE (SAND) | Dominat lithology; relative abundance | 10 | 30 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 |
0.37 | 62-465-1-1,37 | 0 | 0 | 0 | Pleistocene | MAINLY CLAY MINERALS | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 5 | 5 | 0 | 60 | 0 | 0 | 0 | 0 | 0 |
0.38 | 62-465-1-1,38 | 40 | 40 | 20 | Pleistocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 5 | 50 | 45 | 2 | 0 | 0 | 2 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
0.50 | 62-465-1-1,50 | 0 | 0 | 0 | Pleistocene | NANNO-FORAM OOZE | Dominat lithology; relative abundance | 5 | 60 | 34 | 0 | 0 | 0 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
0.63 | 62-465-1-1,63 | 0 | 0 | 0 | Pleistocene | CONSIST MAINLY OF CLAY MINS INS FRACT. | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 30 | 0 | 0 | 5 | 5 | 0 | 60 | 0 | 0 | 0 | 0 | 0 |
0.95 | 62-465-1-CC,0 | 0 | 0 | 0 | Pleistocene | NANNO FORAM OOZE | Dominat lithology; numerical abundance | 6 | 59 | 35 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1.19 | 62-465-2-1,19 | 0 | 0 | 0 | Pleistocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 5 | 55 | 40 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1.60 | 62-465-2-1,60 | 0 | 0 | 0 | Pleistocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 0 | 68 | 32 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 |
2.20 | 62-465-2-11,120 | 0 | 0 | 0 | Pleistocene | NANNO OOZE | Dominat lithology; relative abundance | 20 | 75 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
2.70 | 62-465-2-2,20 | 0 | 0 | 0 | Pliocene | FORAM-NANNO OOZE | Dominat lithology; numerical abundance | 5 | 80 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
3.80 | 62-465-2-21,130 | 0 | 0 | 0 | Pliocene | NANNO OOZE | Dominat lithology; relative abundance | 15 | 80 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
4.30 | 62-465-2-3,30 | 0 | 0 | 0 | Pliocene | NANNO OOZE | Dominat lithology; relative abundance | 10 | 88 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
4.43 | 62-465-2-3,43 | 0 | 0 | 0 | Pliocene | NANNO OOZE (GREENISH YELLOW) | Minor lithology; numerical abundance | 15 | 80 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
5.30 | 62-465-2-31,130 | 0 | 0 | 0 | Tertiary | NANNO OOZE | Dominat lithology; relative abundance | 15 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
5.90 | 62-465-2-4,40 | 0 | 0 | 0 | Tertiary | NANNO OOZE | Dominat lithology; numerical abundance | 4 | 91 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.30 | 62-465-2-4,80 | 0 | 0 | 0 | Tertiary | NANNO OOZE | Dominat lithology; numerical abundance | 10 | 88 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
7.45 | 62-465-2-5,45 | 0 | 0 | 0 | Tertiary | FORAM NANNO OOZE | Minor lithology; numerical abundance | 0 | 82 | 15 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
8.90 | 62-465-2-6,40 | 0 | 0 | 0 | Tertiary | NANNO OOZE | Dominat lithology; numerical abundance | 10 | 85 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
9.34 | 62-465-2-CC,23 | 0 | 0 | 0 | Upper paleocene | CHERTY NANNO OOZE | Minor lithology; relative abundance | 10 | 60 | 2 | 0 | 0 | 30 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
10.55 | 62-465-3-1,5 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Minor lithology; relative abundance | 20 | 72 | 8 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
11.50 | 62-465-3-11,100 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Dominat lithology; numerical abundance | 10 | 90 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
15.40 | 62-465-3-4,40 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 100 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
20.03 | 62-465-4-1,3 | 0 | 0 | 0 | Upper paleocene | SMECTITE CLAY (YELLOWISH GREEN) | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 88 | 0 | 0 | 5 | 0 | 0 |
20.51 | 62-465-4-1,51 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE (GREENISH BLACK BLEB) | Minor lithology; numerical abundance | 1 | 88 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | 0 | 0 | 0 |
22.25 | 62-465-4-2,75 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE (WHITE) | Dominat lithology; numerical abundance | 5 | 90 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
22.67 | 62-465-4-21,117 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Minor lithology; numerical abundance | 15 | 80 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
31.80 | 62-465-5-2,80 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 100 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
34.80 | 62-465-5-4,80 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Dominat lithology; relative abundance | 1 | 97 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
39.70 | 62-465-6-1,70 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Dominat lithology; relative abundance | 2 | 95 | 5 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
42.70 | 62-465-6-3,70 | 0 | 0 | 0 | Upper paleocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 93 | 7 | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
77.70 | 62-465-10-1,70 | 0 | 0 | 0 | Upper maestrichtian | NANNO OOZE | Dominat lithology; numerical abundance | 1 | 93 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
80.10 | 62-465-10-3,10 | 0 | 0 | 0 | Upper maestrichtian | NANNO OOZE | Dominat lithology; numerical abundance | 0 | 94 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
82.20 | 62-465-10-4,70 | 0 | 0 | 0 | Upper maestrichtian | FORAM NANNO OOZE | Dominat lithology; numerical abundance | 3 | 82 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
84.20 | 62-465-10-51,120 | 0 | 0 | 0 | Upper maestrichtian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 96 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
86.60 | 62-465-11-1,10 | 0 | 0 | 0 | Maestrichtian | RECRYSTALLIZED NANNO OOZE | Dominat lithology; numerical abundance | 65 | 25 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
86.97 | 62-465-11-CC,20 | 0 | 0 | 0 | Maestrichtian | TUFF | Minor lithology; numerical abundance | 25 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 60 | 0 |