Larson, Roger L; Moberly, Ralph (2005): Smear slide analysis of Hole 32-310 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230619
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: 36.868500 * Longitude: 176.901500
Date/Time Start: 1973-09-19T00:00:00 * Date/Time End: 1973-09-19T00:00:00
Minimum DEPTH, sediment/rock: 0.03 m * Maximum DEPTH, sediment/rock: 188.10 m
Event(s):
32-310 * Latitude: 36.868500 * Longitude: 176.901500 * Date/Time: 1973-09-19T00:00:00 * Elevation: -3516.0 m * Penetration: 193.5 m * Recovery: 145.2 m * Location: North Pacific/CONT RISE * Campaign: Leg32 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 21 cores; 193.5 m cored; 0 m drilled; 75.1 % 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 | Dolomite | Dol | % | 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 | Zeolite | Zeo | % | Smear slide analysis | ||
18 | Clay minerals | Clay min | % | Smear slide analysis | ||
19 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
20 | Iron | Fe | % | Smear slide analysis | ||
21 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
22 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1197 data points
Data
1 Depth sed [m] | 2 Sample label | 3 Sand [%] | 4 Silt [%] | 5 <2 µm [%] | 6 Stratigraphy | 7 Lithology | 8 Comment | 9 Dol [%] | 10 Nannos [%] | 11 Foram [%] | 12 Rad [%] | 13 Diatoms [%] | 14 Silicoflag [%] | 15 Spiculae [%] | 16 Qz [%] | 17 Zeo [%] | 18 Clay min [%] | 19 Py [%] | 20 Fe [%] | 21 Volc glass [%] | 22 Micronod [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.03 | 32-310-1-1,3 | 10 | 60 | 60 | Upper quaternary | CLAYEY RAD FORAM BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 29 | 12 | 12 | 29 | 3 | 0 | 0 | 0 | 12 | 0 | 0 | 3 | 0 |
0.60 | 32-310-1-1,60 | 10 | 35 | 60 | Upper quaternary | CLAYEY RAD FORAM BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 36 | 15 | 15 | 15 | 4 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 |
1.70 | 32-310-1-2,20 | 10 | 35 | 60 | Upper quaternary | RAD-DIAT-FORAM BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 39 | 16 | 16 | 16 | 0 | 0 | 0 | 0 | 4 | 0 | 4 | 4 | 0 |
2.50 | 32-310-1-21,100 | 10 | 35 | 60 | Upper quaternary | RAD-DIAT-FORAM BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 23 | 23 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
2.67 | 32-310-1-21,117 | 10 | 35 | 60 | Upper quaternary | FORAM BEARING NANNO OOZE | Minor lithology; relative abundance | 0 | 55 | 23 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
6.10 | 32-310-1-CC,0 | 10 | 35 | 60 | Upper quaternary | RAD-DIAT BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 6 | 23 | 23 | 6 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
6.60 | 32-310-2-1,60 | 10 | 35 | 60 | Upper quaternary | CLAYEY-RAD-DIAT-FORAM BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 23 | 23 | 0 | 6 | 0 | 0 | 0 | 23 | 0 | 0 | 6 | 0 |
10.30 | 32-310-2-31,130 | 10 | 35 | 85 | Upper quaternary | RAD-DIAT BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 1 | 6 | 23 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
11.74 | 32-310-2-41,124 | 10 | 35 | 60 | Upper quaternary | RAD-DIAT BEARING NANNO OOZE | Minor lithology; relative abundance | 0 | 55 | 6 | 23 | 23 | 6 | 0 | 0 | 0 | 0 | 23 | 1 | 0 | 0 |
18.00 | 32-310-3-21,100 | 10 | 35 | 60 | Upper quaternary | RAD-DIAT-FORAM BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 39 | 16 | 16 | 16 | 4 | 0 | 0 | 0 | 4 | 0 | 0 | 4 | 0 |
22.50 | 32-310-3-51,100 | 10 | 35 | 60 | Cenozoic | RAD-DIAT-FORAM BEARING NANNO OOZE | Dominat lithology; relative abundance | 6 | 55 | 23 | 23 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
25.61 | 32-310-4-1,61 | 10 | 35 | 60 | Cenozoic | CLAYEY FORAM DIAT RAD BEARING NANNO OOZE | Minor lithology; relative abundance | 0 | 23 | 23 | 23 | 23 | 6 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 |
26.92 | 32-310-4-2,42 | 10 | 35 | 85 | Cenozoic | FORAM BEARING NANNO OOZE | Minor lithology; relative abundance | 0 | 55 | 23 | 6 | 6 | 6 | 0 | 6 | 0 | 6 | 0 | 0 | 6 | 0 |
27.32 | 32-310-4-2,82 | 35 | 35 | 60 | Cenozoic | CLAYEY FORAM-DIAT-RAD BEARING NANNO OOZE | Minor lithology; numerical abundance | 0 | 36 | 15 | 15 | 15 | 4 | 0 | 0 | 0 | 15 | 0 | 0 | 0 | 0 |
30.40 | 32-310-4-4,90 | 10 | 35 | 60 | Pliocene | RAD-DIAT-FORAM BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 39 | 16 | 16 | 16 | 4 | 0 | 0 | 0 | 4 | 0 | 0 | 4 | 0 |
30.70 | 32-310-4-41,120 | 0 | 0 | 0 | Pliocene | CLAYEY FORAM BEARING RAD-DIAT-NANNO OOZE | Dominat lithology; numerical abundance | 0 | 25 | 10 | 25 | 25 | 3 | 0 | 0 | 0 | 10 | 0 | 0 | 3 | 0 |
30.90 | 32-310-4-41,140 | 0 | 0 | 0 | Pliocene | RAD NANNO OOZE | Dominat lithology; numerical abundance | 0 | 29 | 3 | 29 | 12 | 3 | 0 | 0 | 0 | 12 | 0 | 0 | 12 | 0 |
34.10 | 32-310-4-CC,0 | 10 | 35 | 60 | Pliocene | RAD-DIAT BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 6 | 23 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
34.60 | 32-310-5-1,10 | 10 | 35 | 60 | Pliocene | RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 6 | 23 | 6 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 |
43.60 | 32-310-5-CC,0 | 10 | 35 | 60 | Neogene | RAD DIAT BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 6 | 23 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
44.86 | 32-310-6-1,86 | 10 | 35 | 60 | Neogene | CLAYEY RAD-NANNO OOZE | Dominat lithology; numerical abundance | 0 | 32 | 3 | 32 | 13 | 3 | 0 | 0 | 0 | 13 | 0 | 0 | 3 | 0 |
46.50 | 32-310-6-21,100 | 0 | 35 | 85 | Neogene | RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 23 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
57.20 | 32-310-7-3,70 | 0 | 35 | 85 | Upper miocene | CLAYEY RAD BEARING NANNO OOZE | Dominat lithology; numerical abundance | 0 | 39 | 4 | 16 | 16 | 4 | 0 | 0 | 0 | 16 | 0 | 0 | 4 | 0 |
58.65 | 32-310-7-4,65 | 10 | 35 | 60 | Upper miocene | CLAYEY SILICEOUS OOZE | Dominat lithology; numerical abundance | 0 | 10 | 2 | 23 | 23 | 10 | 0 | 0 | 0 | 23 | 0 | 0 | 10 | 0 |
61.10 | 32-310-7-CC,0 | 0 | 35 | 85 | Upper miocene | RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 6 | 23 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
67.00 | 32-310-8-3,50 | 10 | 35 | 60 | Upper miocene | CLAYEY NANNO SILICEOUS OOZE | Dominat lithology; numerical abundance | 0 | 27 | 3 | 27 | 12 | 3 | 0 | 0 | 0 | 27 | 0 | 0 | 0 | 0 |
67.90 | 32-310-8-31,140 | 10 | 35 | 85 | Upper miocene | RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 23 | 6 | 6 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
72.60 | 32-310-8-CC,0 | 10 | 35 | 60 | Upper miocene | RAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 23 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 |
75.50 | 32-310-9-21,100 | 10 | 35 | 60 | Middle miocene | RRAD BEARING NANNO OOZE | Dominat lithology; relative abundance | 6 | 55 | 6 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 6 |
80.00 | 32-310-9-51,100 | 10 | 35 | 60 | Middle miocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
80.42 | 32-310-9-51,142 | 35 | 60 | 60 | Middle miocene | CLAYEY ZEOLITIC NANNO OOZE | Dominat lithology; numerical abundance | 0 | 28 | 11 | 3 | 0 | 0 | 0 | 0 | 11 | 11 | 0 | 11 | 11 | 11 |
80.70 | 32-310-9-6,20 | 0 | 35 | 60 | Lower oligocene | CLAYEY ZEOLITIC NANNO OOZE | Dominat lithology; numerical abundance | 3 | 31 | 3 | 3 | 0 | 0 | 0 | 0 | 13 | 31 | 0 | 13 | 3 | 0 |
82.10 | 32-310-9-CC,0 | 0 | 35 | 85 | Lower oligocene | ZEOLITIC NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 6 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 6 | 0 |
84.50 | 32-310-10-21,100 | 0 | 35 | 85 | Lower oligocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 |
91.10 | 32-310-10-CC,0 | 35 | 60 | 60 | Eocene | ZEOLITIC CLAY WITH NANNOS | Dominat lithology; numerical abundance | 4 | 15 | 4 | 4 | 0 | 0 | 0 | 0 | 36 | 36 | 0 | 0 | 0 | 0 |
94.70 | 32-310-11-3,70 | 0 | 35 | 60 | Eocene | CLAYEY ZEOLITIC NANNO OOZE | Dominat lithology; numerical abundance | 0 | 34 | 4 | 0 | 0 | 0 | 0 | 0 | 14 | 14 | 0 | 14 | 4 | 14 |
98.60 | 32-310-11-CC,0 | 0 | 60 | 60 | Eocene | ZEOLITIC NANNO RICH CLAY | Dominat lithology; numerical abundance | 0 | 30 | 0 | 0 | 0 | 0 | 0 | 0 | 12 | 30 | 0 | 12 | 3 | 12 |
101.15 | 32-310-12-1,65 | 0 | 35 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 |
104.25 | 32-310-12-3,75 | 0 | 35 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
108.10 | 32-310-12-CC,0 | 0 | 35 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 |
114.25 | 32-310-13-3,75 | 0 | 35 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
115.95 | 32-310-13-4,95 | 0 | 35 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
118.94 | 32-310-13-6,94 | 0 | 35 | 85 | Upper senonian | NANNO BEARING FERRUGENOUS CLAY | Minor lithology; numerical abundance | 0 | 16 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 38 | 0 | 38 | 0 | 4 |
119.60 | 32-310-13-CC,0 | 0 | 35 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
125.25 | 32-310-14-4,75 | 0 | 35 | 85 | Upper senonian | SLIGHTLY FERRUGENOUS NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 |
129.10 | 32-310-14-CC,0 | 0 | 35 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 |
131.25 | 32-310-15-2,75 | 0 | 10 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
132.10 | 32-310-15-CC,0 | 0 | 10 | 85 | Upper senonian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
143.90 | 32-310-16-4,90 | 0 | 35 | 85 | Lower campanian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
144.60 | 32-310-16-CC,0 | 0 | 35 | 85 | Lower campanian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 6 | 6 | 0 |
151.75 | 32-310-17-3,75 | 10 | 35 | 85 | Lower campanian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
157.10 | 32-310-17-CC,0 | 0 | 35 | 85 | Lower campanian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 6 |
163.60 | 32-310-18-CC,0 | 0 | 35 | 85 | Lower campanian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
166.60 | 32-310-19-CC,0 | 35 | 35 | 60 | Lower campanian | FORAM BEARING NANNO OOZE | Dominat lithology; relative abundance | 0 | 55 | 23 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 |
177.34 | 32-310-20-2,34 | 0 | 35 | 85 | Lower campanian | NANNO OOZE | Dominat lithology; relative abundance | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
181.60 | 32-310-20-CC,0 | 0 | 35 | 85 | Lower campanian | VOLCANOGENIC CLAYSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 46 | 23 | 0 |
188.10 | 32-310-21-CC,0 | 35 | 60 | 60 | Lower campanian | RAD-DIAT-FORAM-NANNO OOZE | Dominat lithology; numerical abundance | 0 | 23 | 10 | 23 | 23 | 3 | 3 | 0 | 0 | 10 | 0 | 3 | 3 | 0 |