Lewis, Brian T R; Robinson, Paul T (2005): Smear slide analysis of Hole 65-482B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230925
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
Zolotarev, Boris P; Stephen, Ralph A; Schmincke, Hans-Ulrich; Salisbury, Matthew H; Rangin, Claude; Morrison, M Ann; Kudo, A M; Hattner, J; Gutiérrez-Estrada, Mario; Flower, Martin F J; Duennebier, Frederick K; Day, Ron; Cambon, P; Blackinton, Grant; Benson, Richard N; Lewis, Brian T R; Robinson, P (1983): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXV, 752 pp, https://doi.org/10.2973/dsdp.proc.65.1983
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 22.789700 * Longitude: -107.993300
Date/Time Start: 1979-01-24T00:00:00 * Date/Time End: 1979-01-24T00:00:00
Minimum DEPTH, sediment/rock: 44.23 m * Maximum DEPTH, sediment/rock: 224.50 m
Event(s):
65-482B * Latitude: 22.789700 * Longitude: -107.993300 * Date/Time: 1979-01-24T00:00:00 * Elevation: -2998.0 m * Penetration: 229 m * Recovery: 99.8 m * Location: North Pacific/Gulf of California/CONT RISE * Campaign: Leg65 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 24 cores; 184.5 m cored; 0 m drilled; 54.1 % 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 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
15 | Spiculae | Spiculae | % | Smear slide analysis | ||
16 | Quartz | Qz | % | Smear slide analysis | ||
17 | Feldspar | Fsp | % | Smear slide analysis | ||
18 | Zeolite | Zeo | % | Smear slide analysis | ||
19 | Mica | Mica | % | 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 | Heavy minerals | HM | % | Smear slide analysis | ||
25 | Zircon | Zrn | % | Smear slide analysis | ||
26 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
27 | Palagonite | Palagonite | % | Smear slide analysis | ||
28 | Terrigenous | Terr | % | Smear slide analysis | terrigeneous detritus | |
29 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1303 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 Silicoflag [%] | 15 Spiculae [%] | 16 Qz [%] | 17 Fsp [%] | 18 Zeo [%] | 19 Mica [%] | 20 Clay min [%] | 21 Glt [%] | 22 Py [%] | 23 Fe [%] | 24 HM [%] | 25 Zrn [%] | 26 Volc glass [%] | 27 Palagonite [%] | 28 Terr [%] | 29 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
44.23 | 65-482B-1-1,23 | 2 | 38 | 60 | Upper quaternary | Dominat lithology; relative abundance | 0 | 7 | 1 | 0 | 5 | 0 | 5 | 10 | 10 | 0 | 2 | 68 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | |
50.03 | 65-482B-1-5,3 | 1 | 25 | 74 | Upper quaternary | Minor lithology; relative abundance | 2 | 5 | 2 | 0 | 0 | 0 | 10 | 1 | 1 | 0 | 0 | 74 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | |
58.75 | 65-482B-2-4,75 | 0 | 25 | 75 | Upper quaternary | Dominat lithology; numerical abundance | 0 | 24 | 0 | 4 | 8 | 0 | 20 | 20 | 20 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | |
63.10 | 65-482B-3-CC,0 | 2 | 34 | 63 | Upper quaternary | numerical abundance | 3 | 3 | 1 | 1 | 4 | 1 | 2 | 9 | 9 | 0 | 0 | 63 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 2 | |
73.25 | 65-482B-4-1,75 | 0 | 50 | 50 | Upper quaternary | SILTY CLAY | numerical abundance | 2 | 9 | 2 | 0 | 1 | 0 | 0 | 10 | 10 | 0 | 0 | 50 | 1 | 0 | 0 | 5 | 0 | 1 | 0 | 0 | 1 |
74.75 | 65-482B-4-2,75 | 2 | 41 | 57 | Upper quaternary | numerical abundance | 2 | 9 | 3 | 1 | 1 | 0 | 1 | 10 | 10 | 0 | 0 | 57 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 4 | |
76.25 | 65-482B-4-3,75 | 5 | 35 | 60 | Upper quaternary | SILTY CLAY | relative abundance | 1 | 5 | 1 | 0 | 1 | 0 | 2 | 15 | 15 | 2 | 2 | 60 | 2 | 0 | 0 | 2 | 2 | 1 | 0 | 0 | 4 |
83.00 | 65-482B-5-1,50 | 5 | 35 | 60 | Upper quaternary | SILTY CLAY | relative abundance | 0 | 15 | 2 | 2 | 2 | 0 | 0 | 9 | 10 | 2 | 2 | 60 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 5 |
86.10 | 65-482B-5-3,60 | 10 | 40 | 50 | Upper quaternary | SAND SILTY CLAY | relative abundance | 0 | 10 | 2 | 0 | 2 | 0 | 0 | 13 | 13 | 0 | 0 | 50 | 2 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | 3 |
92.25 | 65-482B-6-1,75 | 10 | 40 | 50 | Upper quaternary | SILTY CLAY | relative abundance | 0 | 10 | 2 | 0 | 2 | 0 | 0 | 12 | 12 | 2 | 0 | 60 | 2 | 0 | 0 | 1 | 0 | 2 | 2 | 0 | 5 |
92.71 | 65-482B-6-11,121 | 30 | 15 | 55 | Upper quaternary | SANDY SILT | relative abundance | 3 | 7 | 2 | 0 | 2 | 0 | 0 | 42 | 43 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 2 | 0 | 1 |
96.50 | 65-482B-6-4,50 | 60 | 29 | 1 | Upper quaternary | numerical abundance | 12 | 5 | 15 | 5 | 3 | 1 | 1 | 17 | 18 | 0 | 0 | 11 | 0 | 0 | 0 | 2 | 0 | 4 | 0 | 0 | 7 | |
98.10 | 65-482B-6-5,60 | 25 | 20 | 55 | Upper quaternary | SANDY SILT | relative abundance | 0 | 10 | 10 | 2 | 2 | 2 | 0 | 12 | 13 | 0 | 0 | 55 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
98.92 | 65-482B-6-51,142 | 10 | 28 | 62 | Upper quaternary | relative abundance | 0 | 15 | 1 | 8 | 5 | 2 | 0 | 7 | 7 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
99.30 | 65-482B-6-6,30 | 0 | 28 | 72 | Upper quaternary | Dominat lithology; relative abundance | 2 | 36 | 2 | 0 | 8 | 0 | 18 | 18 | 18 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | |
103.10 | 65-482B-7-2,60 | 0 | 15 | 85 | Upper quaternary | Dominat lithology; relative abundance | 5 | 1 | 0 | 0 | 0 | 0 | 2 | 2 | 3 | 0 | 0 | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 5 | |
113.80 | 65-482B-8-3,30 | 10 | 60 | 30 | Upper quaternary | SAND SILTY CLAY | numerical abundance | 7 | 8 | 7 | 0 | 0 | 0 | 0 | 15 | 15 | 0 | 0 | 42 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
114.02 | 65-482B-8-3,52 | 7 | 30 | 63 | Upper quaternary | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 7 | 5 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 10 | 63 | 0 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
114.03 | 65-482B-8-3,53 | 30 | 40 | 30 | Upper quaternary | SAND SILT CLAY | relative abundance | 0 | 10 | 5 | 0 | 0 | 0 | 0 | 31 | 32 | 0 | 2 | 20 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
114.21 | 65-482B-8-3,71 | 2 | 40 | 58 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 2 | 10 | 1 | 0 | 0 | 0 | 0 | 11 | 12 | 0 | 0 | 58 | 0 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 2 |
114.29 | 65-482B-8-3,79 | 0 | 30 | 70 | Upper quaternary | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 12 | 0 | 1 | 0 | 0 | 0 | 7 | 8 | 0 | 0 | 70 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 |
116.94 | 65-482B-8-5,44 | 0 | 12 | 88 | Upper quaternary | CLAY | Dominat lithology; numerical abundance | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 88 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 1 |
120.75 | 65-482B-9-1,75 | 0 | 20 | 80 | Upper quaternary | CLAY OR SILTY CLAY | Dominat lithology; relative abundance | 2 | 6 | 0 | 0 | 0 | 0 | 0 | 5 | 5 | 0 | 0 | 80 | 0 | 0 | 0 | 1 | 0 | 2 | 1 | 0 | 1 |
122.25 | 65-482B-9-2,75 | 0 | 25 | 75 | Upper quaternary | CLAY OR SILTY CLAY | Dominat lithology; numerical abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 10 | 10 | 0 | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
123.30 | 65-482B-9-3,30 | 0 | 36 | 64 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 15 | 15 | 0 | 0 | 64 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 1 |
123.75 | 65-482B-9-3,75 | 0 | 35 | 65 | Upper quaternary | Dominat lithology; relative abundance | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 12 | 13 | 0 | 0 | 65 | 0 | 1 | 0 | 2 | 0 | 0 | 2 | 0 | 1 | |
124.85 | 65-482B-9-4,35 | 0 | 26 | 74 | Upper quaternary | DIATOMACEOUS CLAY | Dominat lithology; relative abundance | 0 | 7 | 2 | 5 | 10 | 2 | 2 | 2 | 2 | 0 | 0 | 74 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
126.80 | 65-482B-9-5,80 | 0 | 30 | 70 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 2 | 5 | 2 | 0 | 2 | 0 | 0 | 10 | 10 | 2 | 1 | 70 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 |
128.55 | 65-482B-9-61,105 | 0 | 15 | 85 | Upper quaternary | CLAY | Dominat lithology; relative abundance | 1 | 10 | 1 | 0 | 2 | 0 | 0 | 2 | 4 | 2 | 0 | 78 | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 |
130.70 | 65-482B-10-11,120 | 0 | 15 | 85 | Upper quaternary | CLAY | Dominat lithology; relative abundance | 2 | 6 | 2 | 2 | 3 | 0 | 0 | 2 | 2 | 0 | 1 | 85 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 |
133.42 | 65-482B-10-3,92 | 0 | 20 | 80 | Upper quaternary | SILTY CLAY TO CLAY | Dominat lithology; relative abundance | 2 | 6 | 1 | 0 | 0 | 0 | 0 | 5 | 6 | 0 | 1 | 80 | 0 | 1 | 0 | 2 | 0 | 0 | 1 | 0 | 0 |
135.14 | 65-482B-10-41,114 | 0 | 20 | 80 | Upper quaternary | Dominat lithology; relative abundance | 2 | 10 | 0 | 0 | 2 | 0 | 2 | 1 | 1 | 0 | 2 | 85 | 0 | 2 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | |
135.72 | 65-482B-10-5,22 | 0 | 90 | 10 | Upper quaternary | CLAY WITH 85% CALCITE RHOMBS | Dominat lithology; numerical abundance | 85 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | 10 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
136.08 | 65-482B-10-5,58 | 0 | 20 | 80 | Upper quaternary | SILTY CLAY TO CLAY | Dominat lithology; numerical abundance | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 7 | 7 | 0 | 0 | 80 | 0 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 1 |
136.50 | 65-482B-10-51,100 | 0 | 35 | 65 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 0 | 12 | 2 | 0 | 0 | 0 | 0 | 8 | 9 | 3 | 2 | 65 | 0 | 5 | 0 | 1 | 0 | 0 | 2 | 0 | 0 |
136.79 | 65-482B-10-51,129 | 1 | 34 | 65 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 0 | 7 | 2 | 0 | 2 | 0 | 0 | 12 | 12 | 2 | 1 | 65 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 |
137.20 | 65-482B-10-6,20 | 0 | 25 | 75 | Upper quaternary | SILTY CLAY | relative abundance | 2 | 7 | 0 | 0 | 0 | 0 | 0 | 5 | 6 | 1 | 0 | 75 | 0 | 5 | 0 | 0 | 0 | 0 | 1 | 0 | 0 |
137.81 | 65-482B-10-6,81 | 0 | 30 | 70 | Upper quaternary | Dominat lithology; relative abundance | 2 | 12 | 2 | 0 | 2 | 0 | 0 | 5 | 5 | 2 | 0 | 70 | 0 | 6 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | |
138.44 | 65-482B-10-61,144 | 0 | 35 | 65 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 1 | 10 | 1 | 0 | 1 | 0 | 0 | 7 | 8 | 1 | 2 | 65 | 0 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
184.04 | 65-482B-18-1,4 | 0 | 20 | 80 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 1 | 15 | 1 | 0 | 0 | 0 | 0 | 2 | 3 | 0 | 0 | 80 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
193.10 | 65-482B-19-1,10 | 0 | 30 | 70 | Upper quaternary | SILTY CLAYSTONE | Dominat lithology; relative abundance | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 15 | 15 | 0 | 0 | 70 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 2 |
193.15 | 65-482B-19-1,15 | 0 | 30 | 70 | Upper quaternary | SILTY CLAYSTONE | Dominat lithology; relative abundance | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 8 | 9 | 10 | 0 | 70 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 2 |
193.34 | 65-482B-19-1,34 | 2 | 35 | 63 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 14 | 15 | 1 | 0 | 63 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
193.50 | 65-482B-19-1,50 | 0 | 30 | 70 | Upper quaternary | Dominat lithology; relative abundance | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 6 | 7 | 5 | 2 | 70 | 0 | 3 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | |
193.60 | 65-482B-19-1,60 | 0 | 40 | 60 | Upper quaternary | SILTY CLAYSTONE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 15 | 10 | 0 | 60 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
202.00 | 65-482B-21-1,0 | 0 | 25 | 75 | Upper quaternary | SILTY CLAY-COULD BE CONTAMINATION | Minor lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 12 | 13 | 0 | 2 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
224.50 | 65-482B-24-1,0 | 0 | 35 | 65 | Upper quaternary | SILTY CLAY | Dominat lithology; relative abundance | 2 | 12 | 2 | 0 | 2 | 0 | 0 | 11 | 12 | 0 | 0 | 65 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |