Curray, Joseph R; Moore, David G (2005): Smear slide analysis of Hole 64-480 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230920
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
Vacquier, Victor; Simoneit, Bernd R T; Schrader, Hans-Jürgen; Saunders, Andrew D; Rueda-Gaxiola, Jaime; Niemitz, Jeffrey W; Molina-Cruz, Adolfo; Matoba, Y; Lyle, Mitchell W; Kelts, Kerry; Kastner, Miriam; Guerrero-Garcia, Jose; Gieskes, Joris M; Fornari, Daniel J; Einsele, Gerhard; Aubry, Marie-Pierre; Aguayo, J Eduardo; Curray, Joseph R; Moore, David G (1982): Initial Reports of the Deep Sea Drilling Project. U.S. Government Printing Office, LXIV, 507 pp + 1303 pp, https://doi.org/10.2973/dsdp.proc.64.1982
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 27.901700 * Longitude: -111.655700
Date/Time Start: 1978-12-31T00:00:00 * Date/Time End: 1978-12-31T00:00:00
Minimum DEPTH, sediment/rock: 1.10 m * Maximum DEPTH, sediment/rock: 134.15 m
Event(s):
64-480 * Latitude: 27.901700 * Longitude: -111.655700 * Date/Time: 1978-12-31T00:00:00 * Elevation: -655.0 m * Penetration: 152.1 m * Recovery: 117.3 m * Location: North Pacific/Gulf of California/BASIN * Campaign: Leg64 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 30 cores; 144 m cored; 4.8 m drilled; 81.5 % 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 | Chert | Chert | % | Smear slide analysis | fragments | |
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 | Mica | Mica | % | Smear slide analysis | ||
21 | Biotite | Bt | % | Smear slide analysis | ||
22 | Clay minerals | Clay min | % | Smear slide analysis | ||
23 | Opaque minerals | Opaque | % | Smear slide analysis | ||
24 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
25 | Iron | Fe | % | Smear slide analysis | ||
26 | Heavy minerals | HM | % | Smear slide analysis | ||
27 | Hornblende | Hbl | % | Smear slide analysis | ||
28 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
29 | Manganese | Mn | % | Smear slide analysis | ||
30 | Rock fragments | Rock fragm | % | Smear slide analysis | ||
31 | Minerals | Minerals | % | Smear slide analysis | isotropic minerals |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
839 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 Chert [%] | 13 Rad [%] | 14 Diatoms [%] | 15 Silicoflag [%] | 16 Spiculae [%] | 17 Qz [%] | 18 Fsp [%] | 19 Zeo [%] | 20 Mica [%] | 21 Bt [%] | 22 Clay min [%] | 23 Opaque [%] | 24 Py [%] | 25 Fe [%] | 26 HM [%] | 27 Hbl [%] | 28 Volc glass [%] | 29 Mn [%] | 30 Rock fragm [%] | 31 Minerals [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.10 | 64-480-1-11,110 | 0 | 40 | 30 | Quaternary | DIAT OOZE | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 45 | 2 | 1 | 1 | 1 | 0 | 1 | 0 | 20 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
1.10 | 64-480-1-11,110 | 0 | 70 | 60 | Quaternary | MUD DIAT OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 75 | 3 | 1 | 0 | 2 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
10.70 | 64-480-3-11,120 | 0 | 40 | 60 | Quaternary | NANNOFOSSIL DIATOM MUD | Minor lithology; numerical abundance | 2 | 15 | 1 | 0 | 0 | 15 | 0 | 1 | 2 | 4 | 1 | 2 | 0 | 55 | 0 | 1 | 0 | 1 | 0 | 0 | 1 | 0 | 0 |
14.95 | 64-480-4-1,70 | 1 | 44 | 55 | Upper pleistocene | SILTY MUD, NANNO+DIATOM BEARING | Dominat lithology; numerical abundance | 3 | 10 | 0 | 0 | 1 | 10 | 1 | 0 | 6 | 6 | 0 | 3 | 0 | 55 | 0 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 |
15.90 | 64-480-4-2,15 | 0 | 55 | 45 | Upper pleistocene | DIATOMACEOUS SILTY CLAY | Minor lithology; relative abundance | 1 | 2 | 0 | 0 | 2 | 30 | 2 | 2 | 12 | 5 | 0 | 0 | 0 | 45 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
16.45 | 64-480-4-2,70 | 0 | 60 | 40 | Upper pleistocene | DIATOM MUD | Dominat lithology; relative abundance | 3 | 2 | 0 | 0 | 0 | 15 | 0 | 0 | 10 | 8 | 0 | 2 | 0 | 60 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 |
17.95 | 64-480-4-3,70 | 0 | 50 | 55 | Upper pleistocene | NANNO-BEARING SILTY CLAY | Dominat lithology; numerical abundance | 2 | 12 | 0 | 2 | 0 | 8 | 0 | 0 | 10 | 12 | 0 | 0 | 0 | 50 | 0 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 |
32.04 | 64-480-7-3,54 | 0 | 80 | 20 | Upper pleistocene | DIATOMACEOUS OOZE | Minor lithology; relative abundance | 2 | 2 | 0 | 0 | 2 | 80 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 15 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
37.45 | 64-480-8-31,120 | 0 | 50 | 50 | Upper pleistocene | MUDDY DIATOMACEOUS OOZE | Dominat lithology; relative abundance | 1 | 2 | 0 | 0 | 0 | 35 | 2 | 0 | 9 | 2 | 0 | 0 | 0 | 45 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
39.08 | 64-480-9-11,108 | 0 | 0 | 0 | Upper pleistocene | FISH BONE REMAINS IN CLAYEY MATRIX | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 8 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 2 | 1 | 50 | 0 | 0 | 0 | 0 | 0 | 0 |
47.65 | 64-480-11-1,15 | 0 | 55 | 45 | Upper pleistocene | DIATOMACEOUS CLAYEY SILT | Minor lithology; relative abundance | 2 | 0 | 0 | 0 | 2 | 33 | 2 | 2 | 12 | 2 | 0 | 0 | 0 | 45 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
63.91 | 64-480-13-2,66 | 0 | 40 | 60 | Upper pleistocene | DIATOMACEOUS CLAY | Minor lithology; relative abundance | 3 | 2 | 0 | 0 | 2 | 15 | 2 | 0 | 15 | 3 | 0 | 0 | 0 | 60 | 3 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | 0 |
67.50 | 64-480-14-11,100 | 0 | 40 | 60 | Upper pleistocene | CLAYEY DIATOMACEOUS OOZE | Dominat lithology; relative abundance | 3 | 10 | 2 | 0 | 0 | 35 | 0 | 0 | 1 | 2 | 0 | 0 | 0 | 50 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
67.60 | 64-480-14-11,110 | 3 | 62 | 35 | Upper pleistocene | VOLC GLAS BEARING MUDDY DIAT OOZE | Minor lithology; relative abundance | 2 | 8 | 1 | 0 | 0 | 35 | 2 | 0 | 3 | 1 | 0 | 0 | 0 | 28 | 3 | 2 | 0 | 0 | 0 | 20 | 0 | 0 | 0 |
68.70 | 64-480-14-2,70 | 0 | 50 | 50 | Upper pleistocene | MUDDY DIATOMACEOUS OOZE | Dominat lithology; relative abundance | 4 | 12 | 2 | 0 | 0 | 35 | 0 | 0 | 4 | 1 | 0 | 0 | 0 | 45 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
73.40 | 64-480-15-2,65 | 0 | 50 | 50 | Upper pleistocene | DIATOMACEOUS CLAYEY SILTSTONE | Dominat lithology; relative abundance | 4 | 10 | 1 | 0 | 0 | 25 | 0 | 0 | 8 | 3 | 0 | 0 | 0 | 45 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
95.95 | 64-480-20-1,95 | 100 | 0 | 0 | Upper pleistocene | GRAY SAND | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 25 | 60 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 15 | 3 |
101.09 | 64-480-21-11,134 | 0 | 50 | 50 | Upper pleistocene | CALCAREOUS CLAYSTONE | Minor lithology; relative abundance | 45 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 40 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
101.40 | 64-480-21-2,15 | 0 | 50 | 50 | Upper pleistocene | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 4 | 15 | 0 | 0 | 0 | 70 | 0 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | |
101.43 | 64-480-21-2,18 | 0 | 55 | 45 | Upper pleistocene | MUDDY DIATOMACEOUS OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 50 | 3 | 0 | 6 | 1 | 0 | 0 | 0 | 40 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
120.10 | 64-480-25-11,135 | 0 | 20 | 80 | Upper pleistocene | CLAYSTONE | Minor lithology; numerical abundance | 1 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | 8 | 2 | 0 | 0 | 0 | 80 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
124.33 | 64-480-26-1,83 | 0 | 45 | 30 | Upper pleistocene | DIATOMACEOUS OOZE | Minor lithology; relative abundance | 2 | 2 | 2 | 0 | 2 | 40 | 1 | 1 | 1 | 1 | 0 | 1 | 0 | 25 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
124.33 | 64-480-26-1,83 | 0 | 70 | 55 | Upper pleistocene | MUDDY DIATOMACEOUS OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 70 | 0 | 0 | 4 | 1 | 0 | 0 | 0 | 50 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
124.87 | 64-480-26-11,137 | 0 | 35 | 65 | Upper pleistocene | MUDDY DIATOMACEOUS OOZE HARD SPECK | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 45 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 53 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
125.52 | 64-480-26-2,52 | 0 | 0 | 0 | Upper pleistocene | CLAYSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 10 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 85 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
127.13 | 64-480-26-3,63 | 0 | 55 | 45 | Upper pleistocene | MUDDY DIATOMACEOUS OOZE | Minor lithology; relative abundance | 3 | 9 | 2 | 0 | 2 | 40 | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 40 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 |
134.15 | 64-480-28-11,115 | 0 | 70 | 10 | Upper pleistocene | DIATOMACEOUS OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 10 | 1 | 0 | 1 | 1 | 0 | 0 | 0 | 10 | 2 | 2 | 0 | 0 | 0 | 75 | 0 | 0 | 0 |
134.15 | 64-480-28-11,115 | 0 | 90 | 30 | Upper pleistocene | PUMICE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 2 | 72 | 2 | 0 | 2 | 2 | 0 | 0 | 0 | 25 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |