Larson, Roger L; Moberly, Ralph (2005): Smear slide analysis of Hole 32-303 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230611
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
Larson, Roger L; Moberly, Ralph; Bukry, David; Foreman, H P; Gardner, James V; Keene, John B; Lancelot, Yves; Luterbacher, Hanspeter; Marshall, M C; Matter, A (1975): Initial Reports of the Deep Sea Drilling Project. U. S. Government Printing Office, XXXII, 980 pp, https://doi.org/10.2973/dsdp.proc.32.1975
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 40.808300 * Longitude: 154.451200
Date/Time Start: 1973-08-18T00:00:00 * Date/Time End: 1973-08-18T00:00:00
Minimum DEPTH, sediment/rock: 1.60 m * Maximum DEPTH, sediment/rock: 211.10 m
Event(s):
32-303 * Latitude: 40.808300 * Longitude: 154.451200 * Date/Time: 1973-08-18T00:00:00 * Elevation: -5609.0 m * Penetration: 229 m * Recovery: 25.9 m * Location: North Pacific/BASIN * Campaign: Leg32 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 5 cores; 45 m cored; 9 m drilled; 57.6 % 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 | Nannofossils | Nannos | % | Smear slide analysis | ||
10 | Radiolarians | Rad | % | Smear slide analysis | ||
11 | Diatoms | Diatoms | % | Smear slide analysis | ||
12 | Silicoflagellates | Silicoflag | % | Smear slide analysis | ||
13 | Spiculae | Spiculae | % | Smear slide analysis | ||
14 | Quartz | Qz | % | Smear slide analysis | ||
15 | Feldspar | Fsp | % | Smear slide analysis | ||
16 | Zeolite | Zeo | % | Smear slide analysis | ||
17 | Clay minerals | Clay min | % | Smear slide analysis | ||
18 | Iron | Fe | % | Smear slide analysis | ||
19 | Heavy minerals | HM | % | Smear slide analysis | ||
20 | Pyroxene | Pyrox | % | Smear slide analysis | ||
21 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
22 | Palagonite | Palagonite | % | Smear slide analysis | ||
23 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
437 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Nannos [%] | 10 Rad [%] | 11 Diatoms [%] | 12 Silicoflag [%] | 13 Spiculae [%] | 14 Qz [%] | 15 Fsp [%] | 16 Zeo [%] | 17 Clay min [%] | 18 Fe [%] | 19 HM [%] | 20 Pyrox [%] | 21 Volc glass [%] | 22 Palagonite [%] | 23 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1.60 | 32-303-1-CC,0 | 35 | 60 | 60 | Upper pleistocene | DIATOM VOLCANIC ASH | Dominat lithology; numerical abundance | 0 | 12 | 28 | 3 | 0 | 3 | 3 | 0 | 0 | 3 | 0 | 0 | 41 | 3 | 3 |
62.58 | 32-303-2-1,58 | 35 | 60 | 60 | Lower pliocene | RADIOLARIAN DIATOM OOZE | Minor lithology; numerical abundance | 0 | 35 | 35 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
62.66 | 32-303-2-1,66 | 35 | 60 | 60 | Lower pliocene | DIATOM RADIOLARIAN OOZE | Minor lithology; numerical abundance | 0 | 35 | 35 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
62.88 | 32-303-2-1,88 | 35 | 60 | 60 | Lower pliocene | DIATOM RADIOLARIAN OOZE | Dominat lithology; numerical abundance | 0 | 33 | 33 | 14 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 17 | 0 | 0 |
62.98 | 32-303-2-1,98 | 10 | 60 | 60 | Lower pliocene | RADIOLARIAN DIATOM OOZE | Minor lithology; numerical abundance | 0 | 31 | 31 | 13 | 0 | 0 | 0 | 0 | 13 | 0 | 0 | 0 | 13 | 0 | 0 |
64.60 | 32-303-2-21,110 | 35 | 60 | 60 | Lower pliocene | DIATOM RADIOLARIAN OOZE | Dominat lithology; numerical abundance | 0 | 35 | 35 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
64.97 | 32-303-2-21,147 | 35 | 60 | 60 | Lower pliocene | DIATOM RADIOLARIAN OOZE | Dominat lithology; numerical abundance | 0 | 35 | 35 | 15 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 15 | 0 | 0 |
67.17 | 32-303-2-4,67 | 60 | 60 | 10 | Lower pliocene | VOLCANIC ASH | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 81 | 0 | 0 |
71.10 | 32-303-2-CC,0 | 35 | 60 | 60 | DIATOM RADIOLARIAN OOZE | Dominat lithology; numerical abundance | 3 | 32 | 32 | 13 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 13 | 3 | 0 | |
118.38 | 32-303-3-11,138 | 35 | 60 | 60 | Upper miocene | CLAYEY DIATOM RADIOLARIAN OOZE | Dominat lithology; numerical abundance | 0 | 29 | 29 | 12 | 0 | 0 | 0 | 0 | 12 | 3 | 0 | 0 | 15 | 0 | 0 |
119.97 | 32-303-3-21,147 | 35 | 60 | 60 | Upper miocene | CLAYEY DIATOM RADIOLARIAN OOZE | Dominat lithology; numerical abundance | 0 | 30 | 30 | 12 | 0 | 0 | 0 | 0 | 12 | 0 | 0 | 0 | 15 | 0 | 0 |
123.75 | 32-303-3-5,75 | 35 | 85 | 10 | Upper miocene | VOLCANIC ASH | Minor lithology; relative abundance | 0 | 6 | 6 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 6 | 75 | 6 | 0 |
123.90 | 32-303-3-5,90 | 10 | 60 | 35 | Upper miocene | CLAYEY DIATOM RAD OOZE | Dominat lithology; numerical abundance | 0 | 31 | 31 | 13 | 0 | 0 | 0 | 0 | 13 | 0 | 0 | 0 | 13 | 0 | 0 |
126.10 | 32-303-3-CC,0 | 10 | 85 | 35 | Upper miocene | ASH RICH DIATOM RAD OOZE | Dominat lithology; numerical abundance | 0 | 25 | 25 | 10 | 0 | 3 | 0 | 0 | 10 | 0 | 0 | 0 | 28 | 0 | 0 |
176.15 | 32-303-4-2,65 | 0 | 60 | 60 | Upper miocene | RAD RICH RED CLAY WITH FERROMANGANESEMICRO NODULES | Minor lithology; numerical abundance | 0 | 38 | 4 | 4 | 0 | 0 | 0 | 0 | 38 | 0 | 0 | 0 | 0 | 0 | 16 |
176.30 | 32-303-4-2,80 | 10 | 60 | 60 | Upper miocene | RAD RICH RED CLAY | Dominat lithology; numerical abundance | 0 | 33 | 14 | 14 | 0 | 0 | 0 | 0 | 33 | 0 | 0 | 0 | 3 | 0 | 3 |
177.66 | 32-303-4-3,66 | 0 | 60 | 60 | Upper miocene | RAD BEARING RED CLAY | Minor lithology; relative abundance | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 6 |
183.10 | 32-303-4-CC,0 | 0 | 35 | 85 | RAD BEARING RED CLAY | Dominat lithology; numerical abundance | 0 | 15 | 4 | 0 | 0 | 0 | 0 | 4 | 50 | 15 | 0 | 0 | 6 | 4 | 0 | |
183.10 | 32-303-4-CC,0 | 0 | 35 | 85 | RAD BEARING RED CLAY | Dominat lithology; relative abundance | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 75 | 0 | 0 | 0 | 8 | 0 | 0 | |
211.10 | 32-303-5-CC,0 | 0 | 35 | 60 | Cretaceous | SLIGHTLY ZEOLITIC BROWN CLAY | Dominat lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 15 | 48 | 19 | 0 | 0 | 0 | 0 | 15 |