Lewis, Brian T R; Robinson, Paul T (2005): Smear slide analysis of Hole 65-483B. PANGAEA, https://doi.org/10.1594/PANGAEA.230930
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: 22.883200 * Longitude: -108.747300
Date/Time Start: 1979-02-12T00:00:00 * Date/Time End: 1979-02-12T00:00:00
Minimum DEPTH, sediment/rock: 91.91 m * Maximum DEPTH, sediment/rock: 237.02 m
Event(s):
65-483B * Latitude: 22.883200 * Longitude: -108.747300 * Date/Time: 1979-02-12T00:00:00 * Elevation: -3070.0 m * Penetration: 267 m * Recovery: 91.8 m * Location: North Pacific/Gulf of California/CONT RISE * Campaign: Leg65 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 28 cores; 160.5 m cored; 28.5 m drilled; 57.2 % 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 | Barite | Brt | % | Smear slide analysis | ||
15 | Quartz | Qz | % | Smear slide analysis | ||
16 | Feldspar | Fsp | % | Smear slide analysis | ||
17 | Zeolite | Zeo | % | Smear slide analysis | ||
18 | Mica | Mica | % | Smear slide analysis | ||
19 | Clay minerals | Clay min | % | Smear slide analysis | ||
20 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
21 | Heavy minerals | HM | % | Smear slide analysis | ||
22 | Pyroxene | Pyrox | % | Smear slide analysis | ||
23 | Volcanic glass | Volc glass | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
588 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 Brt [%] | 15 Qz [%] | 16 Fsp [%] | 17 Zeo [%] | 18 Mica [%] | 19 Clay min [%] | 20 Py [%] | 21 HM [%] | 22 Pyrox [%] | 23 Volc glass [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
91.91 | 65-483B-1-1,41 | 3 | 11 | 86 | Quaternary | CLAY (SILTY CLAY) | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 7 | 3 | 0 | 2 | 86 | 1 | 1 | 0 | 0 |
92.34 | 65-483B-1-1,84 | 0 | 10 | 90 | Quaternary | SILTY CLAY | Minor lithology; relative abundance | 0 | 3 | 2 | 0 | 0 | 2 | 4 | 2 | 0 | 0 | 90 | 0 | 1 | 0 | 0 |
92.61 | 65-483B-1-11,111 | 2 | 10 | 88 | Quaternary | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 3 | 0 | 1 | 88 | 1 | 1 | 0 | 0 |
93.64 | 65-483B-1-2,64 | 0 | 15 | 85 | Quaternary | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 2 | 0 | 0 | 7 | 3 | 0 | 1 | 85 | 1 | 1 | 0 | 0 |
94.47 | 65-483B-1-21,147 | 0 | 10 | 90 | Quaternary | CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 1 | 90 | 1 | 2 | 0 | 0 |
95.15 | 65-483B-1-3,65 | 0 | 14 | 86 | Quaternary | SILTY CLAY | Dominat lithology; numerical abundance | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | 1 | 86 | 0 | 0 | 0 | 3 |
96.65 | 65-483B-1-4,65 | 0 | 12 | 88 | Quaternary | CLAY (SILTY CLAY) | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | 1 | 88 | 0 | 1 | 0 | 3 |
97.98 | 65-483B-1-5,48 | 0 | 12 | 88 | Quaternary | CLAY (SILTY CLAY) | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 3 | 0 | 0 | 88 | 0 | 2 | 0 | 1 |
98.14 | 65-483B-1-5,64 | 10 | 6 | 84 | Quaternary | SANDY CLAY | relative abundance | 0 | 0 | 2 | 0 | 0 | 0 | 8 | 2 | 0 | 0 | 84 | 1 | 3 | 0 | 2 |
101.75 | 65-483B-2-1,75 | 0 | 15 | 85 | Quaternary | CLAY (SILT CLAY) | Dominat lithology; relative abundance | 2 | 2 | 0 | 0 | 0 | 0 | 6 | 3 | 0 | 1 | 85 | 0 | 5 | 0 | 0 |
103.25 | 65-483B-2-2,75 | 0 | 12 | 88 | Quaternary | CLAY (SILT CLAY) | Dominat lithology; relative abundance | 2 | 1 | 0 | 2 | 0 | 0 | 5 | 2 | 0 | 0 | 88 | 0 | 3 | 0 | 1 |
104.75 | 65-483B-2-3,75 | 0 | 8 | 92 | Quaternary | CLAY | Dominat lithology; numerical abundance | 0 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 92 | 0 | 4 | 0 | 0 |
105.53 | 65-483B-2-4,3 | 3 | 5 | 92 | Quaternary | CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 0 | 92 | 0 | 2 | 0 | 2 |
106.25 | 65-483B-2-4,75 | 0 | 14 | 86 | Quaternary | CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 0 | 0 | 7 | 3 | 0 | 0 | 86 | 0 | 4 | 0 | 0 |
107.75 | 65-483B-2-5,75 | 0 | 10 | 90 | Quaternary | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 1 | 0 | 0 | 90 | 1 | 3 | 0 | 1 | |
109.25 | 65-483B-2-6,75 | 1 | 90 | 9 | Quaternary | Dominat lithology; relative abundance | 74 | 0 | 0 | 0 | 0 | 0 | 15 | 1 | 0 | 0 | 9 | 0 | 1 | 2 | 2 | |
133.03 | 65-483B-7-1,3 | 0 | 18 | 82 | SILTY CLAY | Dominat lithology; relative abundance | 2 | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 2 | 82 | 1 | 2 | 0 | 5 | |
137.54 | 65-483B-8-1,4 | 0 | 16 | 84 | SILTY CLAY | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 1 | 0 | 7 | 3 | 0 | 0 | 84 | 3 | 2 | 0 | 2 | |
146.53 | 65-483B-9-1,3 | 0 | 23 | 77 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 8 | 0 | 0 | 2 | 0 | 7 | 2 | 0 | 0 | 77 | 6 | 0 | 0 | 0 |
210.65 | 65-483B-20-2,65 | 0 | 5 | 95 | Upper pliocene | CLAY (ALTERED VOLCANIC GLASS) | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 2 | 0 | 95 | 0 | 0 | 0 | 0 |
210.67 | 65-483B-20-2,67 | 0 | 6 | 94 | Upper pliocene | CLAY | Dominat lithology; relative abundance | 0 | 2 | 0 | 0 | 2 | 0 | 4 | 2 | 0 | 0 | 94 | 0 | 0 | 0 | 2 |
210.98 | 65-483B-20-2,98 | 3 | 10 | 87 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 2 | 7 | 0 | 2 | 2 | 0 | 3 | 1 | 0 | 0 | 87 | 1 | 3 | 0 | 5 |
211.02 | 65-483B-20-21,102 | 0 | 16 | 84 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 2 | 4 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | 0 | 84 | 2 | 4 | 0 | 2 |
211.12 | 65-483B-20-21,112 | 0 | 13 | 87 | Upper pliocene | SILTY CLAY | relative abundance | 0 | 3 | 2 | 2 | 2 | 0 | 4 | 1 | 0 | 2 | 87 | 0 | 5 | 0 | 0 |
211.28 | 65-483B-20-21,128 | 1 | 12 | 87 | Upper pliocene | SILTY CLAY | Dominat lithology; relative abundance | 0 | 3 | 0 | 2 | 0 | 0 | 3 | 1 | 0 | 0 | 87 | 1 | 5 | 0 | 2 |
232.64 | 65-483B-25-2,14 | 0 | 23 | 77 | SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 3 | 0 | 0 | 77 | 0 | 10 | 0 | 2 | |
237.02 | 65-483B-26-2,2 | 0 | 12 | 88 | SILTY CLAYSTONE | Dominat lithology; relative abundance | 0 | 5 | 0 | 0 | 0 | 0 | 6 | 1 | 0 | 0 | 88 | 0 | 0 | 0 | 2 |