Prell, Warren L; Gardner, James V (2005): Smear slide analysis of Hole 68-502B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230965
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
Zimmerman, Herman; Spariosu, Dann J; Sancetta, Constance A; Riedel, William R; Mayer, Larry A; Mann, Ulrich; Ledbetter, Michael T; Kent, Dennis V; Keigwin, Lloyd D; Fleet, A J; Blechschmidt, G; Adelseck, C; Prell, Warren L; Gardner, James V (1982): Initial Reports of the Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, LXVIII, 495 pp, https://doi.org/10.2973/dsdp.proc.68.1982
Further details:
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 11.491800 * Longitude: -79.378200
Date/Time Start: 1979-08-16T00:00:00 * Date/Time End: 1979-08-16T00:00:00
Minimum DEPTH, sediment/rock: 0.80 m * Maximum DEPTH, sediment/rock: 96.40 m
Event(s):
68-502B * Latitude: 11.491800 * Longitude: -79.378200 * Date/Time: 1979-08-16T00:00:00 * Elevation: -3051.0 m * Penetration: 99.7 m * Recovery: 87.7 m * Location: Caribbean Sea/RIDGE * Campaign: Leg68 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 99.7 m cored; 0 m drilled; 88 % 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 | Spiculae | Spiculae | % | Smear slide analysis | ||
| 13 | Quartz | Qz | % | Smear slide analysis | ||
| 14 | Zeolite | Zeo | % | Smear slide analysis | ||
| 15 | Mica | Mica | % | Smear slide analysis | ||
| 16 | Clay minerals | Clay min | % | Smear slide analysis | ||
| 17 | Pyrite, FeS2 | Py | % | Smear slide analysis | ||
| 18 | Heavy minerals | HM | % | Smear slide analysis | ||
| 19 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
| 20 | Micronodules | Micronod | % | Smear slide analysis |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
949 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 Spiculae [%] | 13 Qz [%] | 14 Zeo [%] | 15 Mica [%] | 16 Clay min [%] | 17 Py [%] | 18 HM [%] | 19 Volc glass [%] | 20 Micronod [%] |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 0.80 | 68-502B-1-1,80 | 0 | 0 | 0 | Quaternary | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 25 | 15 | 0 | 1 | 0 | 0 | 5 | 1 | 1 | 3 | 2 |
| 1.36 | 68-502B-1-11,136 | 0 | 0 | 0 | Quaternary | MICRONOD & FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 25 | 15 | 0 | 1 | 0 | 0 | 48 | 0 | 1 | 2 | 7 |
| 3.80 | 68-502B-2-1,90 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 25 | 20 | 0 | 1 | 0 | 0 | 47 | 0 | 1 | 3 | 2 |
| 4.87 | 68-502B-2-2,47 | 0 | 0 | 0 | Pleistocene | NANNO-FORAM OOZE | Dominat lithology; numerical abundance | 3 | 30 | 30 | 0 | 1 | 0 | 0 | 30 | 2 | 1 | 3 | 0 |
| 6.40 | 68-502B-2-3,50 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 30 | 20 | 0 | 1 | 0 | 0 | 43 | 0 | 1 | 2 | 2 |
| 8.16 | 68-502B-3-1,86 | 0 | 0 | 0 | Pleistocene | ASH,FORAM & NANNO BEARING MARL | Minor lithology; numerical abundance | 2 | 20 | 15 | 0 | 1 | 0 | 0 | 51 | 3 | 1 | 5 | 2 |
| 8.50 | 68-502B-3-11,120 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 2 | 30 | 20 | 0 | 1 | 0 | 1 | 39 | 1 | 1 | 3 | 2 |
| 9.03 | 68-502B-3-2,23 | 0 | 0 | 0 | Pleistocene | NANNO FORAM OOZE | Dominat lithology; numerical abundance | 5 | 25 | 30 | 0 | 1 | 0 | 0 | 34 | 0 | 1 | 3 | 1 |
| 10.40 | 68-502B-3-3,10 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 3 | 25 | 20 | 0 | 1 | 0 | 0 | 44 | 1 | 1 | 2 | 1 |
| 11.40 | 68-502B-3-31,110 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 30 | 20 | 0 | 1 | 0 | 1 | 41 | 2 | 0 | 3 | 1 |
| 11.75 | 68-502B-4-1,5 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 2 | 30 | 20 | 0 | 1 | 0 | 0 | 41 | 2 | 1 | 2 | 1 |
| 12.80 | 68-502B-4-11,110 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 25 | 20 | 0 | 1 | 0 | 0 | 48 | 1 | 1 | 2 | 1 |
| 14.15 | 68-502B-4-2,95 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Minor lithology; numerical abundance | 2 | 30 | 20 | 0 | 1 | 0 | 0 | 39 | 4 | 1 | 2 | 1 |
| 17.00 | 68-502B-5-1,90 | 0 | 0 | 0 | Pleistocene | NANNO-FORAM MARL | Dominat lithology; numerical abundance | 3 | 25 | 30 | 0 | 1 | 0 | 0 | 37 | 1 | 1 | 2 | 0 |
| 18.33 | 68-502B-5-2,73 | 0 | 0 | 0 | Pleistocene | NANNO BEARING FORAM MARL | Minor lithology; numerical abundance | 2 | 10 | 30 | 0 | 1 | 0 | 0 | 51 | 0 | 2 | 2 | 2 |
| 18.65 | 68-502B-5-21,105 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 30 | 20 | 0 | 1 | 0 | 0 | 43 | 1 | 1 | 3 | 0 |
| 20.02 | 68-502B-5-3,92 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 25 | 15 | 0 | 1 | 0 | 0 | 52 | 2 | 1 | 3 | 0 |
| 20.66 | 68-502B-6-1,16 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 2 | 25 | 20 | 0 | 1 | 0 | 0 | 46 | 1 | 1 | 3 | 1 |
| 22.80 | 68-502B-6-2,80 | 0 | 0 | 0 | Pleistocene | NANNO BEARING FORAM CLAY | Dominat lithology; numerical abundance | 2 | 15 | 25 | 0 | 1 | 0 | 0 | 52 | 1 | 1 | 2 | 1 |
| 28.55 | 68-502B-7-3,65 | 0 | 0 | 0 | Pleistocene | NANNO BEARING FORAM MARL | Dominat lithology; numerical abundance | 3 | 20 | 35 | 0 | 1 | 0 | 0 | 33 | 1 | 21 | 4 | 1 |
| 28.80 | 68-502B-7-3,90 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 25 | 15 | 0 | 1 | 0 | 0 | 50 | 3 | 1 | 3 | 1 |
| 30.25 | 68-502B-8-1,95 | 0 | 0 | 0 | Pleistocene | FORAM & NANNO BEARING MARL | Dominat lithology; numerical abundance | 1 | 20 | 10 | 0 | 1 | 0 | 0 | 62 | 2 | 1 | 3 | 0 |
| 31.20 | 68-502B-8-2,40 | 0 | 0 | 0 | Pleistocene | ZEOL,NANNO,FORAM & ASH BEARING MARL | Minor lithology; numerical abundance | 2 | 15 | 15 | 0 | 1 | 5 | 0 | 42 | 1 | 1 | 18 | 0 |
| 31.26 | 68-502B-8-2,46 | 0 | 0 | 0 | Pleistocene | VITRIC ASH | Minor lithology; numerical abundance | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 97 | 1 |
| 32.10 | 68-502B-8-21,130 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 1 | 25 | 10 | 0 | 1 | 0 | 0 | 55 | 2 | 1 | 4 | 1 |
| 32.60 | 68-502B-8-3,30 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 3 | 25 | 10 | 0 | 1 | 0 | 0 | 58 | 1 | 1 | 1 | 0 |
| 35.10 | 68-502B-9-11,140 | 0 | 0 | 0 | Pleistocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 3 | 25 | 20 | 0 | 1 | 0 | 0 | 46 | 1 | 1 | 2 | 1 |
| 35.53 | 68-502B-9-2,33 | 0 | 0 | 0 | Pleistocene | NANNO BEARING FORAM PYRITITE | Minor lithology; numerical abundance | 2 | 10 | 25 | 0 | 0 | 0 | 0 | 21 | 40 | 1 | 1 | 0 |
| 35.80 | 68-502B-9-2,60 | 0 | 0 | 0 | Pleistocene | NANNO BEARING FORAM MARL | Dominat lithology; numerical abundance | 2 | 15 | 40 | 0 | 1 | 2 | 0 | 35 | 1 | 1 | 3 | 0 |
| 36.80 | 68-502B-9-3,10 | 0 | 0 | 0 | Pleistocene | NANNO BEARING FORAM MARL | Dominat lithology; numerical abundance | 2 | 15 | 30 | 0 | 1 | 0 | 0 | 89 | 1 | 1 | 1 | 0 |
| 41.08 | 68-502B-10-21,148 | 0 | 0 | 0 | Pleistocene | NANNO + FORAM BEARING MARL | Dominat lithology; numerical abundance | 3 | 15 | 20 | 0 | 1 | 0 | 0 | 57 | 1 | 1 | 2 | 0 |
| 43.70 | 68-502B-11-11,120 | 0 | 0 | 0 | Pleistocene | FORAM + NANNO BEARING MARL | Dominat lithology; numerical abundance | 1 | 20 | 15 | 0 | 1 | 0 | 0 | 59 | 1 | 1 | 2 | 0 |
| 44.26 | 68-502B-11-2,26 | 0 | 0 | 0 | Pleistocene | NANNO + FORAM BEARING MARL | Dominat lithology; numerical abundance | 3 | 20 | 20 | 0 | 1 | 0 | 0 | 52 | 1 | 1 | 2 | 0 |
| 50.20 | 68-502B-12-3,30 | 0 | 0 | 0 | Upper pliocene | FORAM + NANNO BEARING MARL | Dominat lithology; numerical abundance | 3 | 20 | 20 | 0 | 1 | 0 | 0 | 53 | 1 | 1 | 1 | 0 |
| 53.61 | 68-502B-13-2,81 | 0 | 0 | 0 | Upper pliocene | FORAM & NANNO BEARING MARL | Dominat lithology; numerical abundance | 1 | 20 | 15 | 0 | 1 | 0 | 0 | 58 | 2 | 1 | 2 | 0 |
| 56.50 | 68-502B-14-1,80 | 0 | 0 | 0 | Upper pliocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 2 | 25 | 10 | 0 | 1 | 0 | 0 | 57 | 1 | 1 | 3 | 0 |
| 57.00 | 68-502B-14-11,130 | 0 | 0 | 0 | Upper pliocene | NANNO BEARING FORAM MARL | Dominat lithology; numerical abundance | 1 | 15 | 25 | 0 | 1 | 0 | 0 | 54 | 1 | 1 | 2 | 0 |
| 60.64 | 68-502B-15-1,54 | 0 | 0 | 0 | Upper pliocene | NANNO BEARING FORAM MARL | Dominat lithology; numerical abundance | 2 | 15 | 30 | 0 | 1 | 0 | 0 | 45 | 2 | 1 | 3 | 1 |
| 61.00 | 68-502B-15-1,90 | 0 | 0 | 0 | Upper pliocene | FORAM + NANNO BEARING MARL | Dominat lithology; numerical abundance | 2 | 20 | 10 | 0 | 1 | 0 | 0 | 63 | 2 | 1 | 1 | 0 |
| 65.30 | 68-502B-16-1,80 | 0 | 0 | 0 | Upper pliocene | FORAM + NANNO BEARING MARL | Dominat lithology; numerical abundance | 2 | 20 | 10 | 0 | 1 | 0 | 0 | 63 | 2 | 1 | 1 | 0 |
| 69.60 | 68-502B-17-1,70 | 0 | 0 | 0 | Upper pliocene | FORAM + NANNO BEARING MARL | Dominat lithology; numerical abundance | 2 | 20 | 15 | 0 | 1 | 0 | 0 | 58 | 1 | 1 | 2 | 0 |
| 71.64 | 68-502B-17-21,124 | 0 | 0 | 0 | Upper pliocene | FORAM + NANNO BEARING MARL | Dominat lithology; numerical abundance | 3 | 20 | 15 | 0 | 1 | 0 | 0 | 53 | 4 | 1 | 3 | 0 |
| 75.40 | 68-502B-18-2,60 | 0 | 0 | 0 | Upper pliocene | NANNO BEARING FORAM MARL | Dominat lithology; numerical abundance | 2 | 20 | 25 | 0 | 1 | 0 | 0 | 48 | 2 | 1 | 1 | 0 |
| 80.00 | 68-502B-19-2,80 | 0 | 0 | 0 | Lower pliocene | NANNO BEARING FORAM MARL | Dominat lithology; numerical abundance | 3 | 15 | 20 | 0 | 1 | 0 | 0 | 47 | 1 | 1 | 2 | 0 |
| 83.20 | 68-502B-20-11,110 | 0 | 0 | 0 | Lower pliocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 3 | 25 | 5 | 0 | 1 | 0 | 0 | 60 | 1 | 1 | 4 | 0 |
| 85.12 | 68-502B-20-3,2 | 0 | 0 | 0 | Lower pliocene | FORAM + NANNO BEARING MARL | Dominat lithology; numerical abundance | 2 | 20 | 8 | 1 | 1 | 0 | 0 | 61 | 3 | 1 | 3 | 0 |
| 85.85 | 68-502B-20-3,75 | 0 | 0 | 0 | Lower pliocene | FORAM,NANNO, PYR BEARING CALC CLAY | Minor lithology; numerical abundance | 3 | 15 | 5 | 0 | 1 | 1 | 0 | 40 | 30 | 1 | 4 | 0 |
| 88.40 | 68-502B-21-2,40 | 0 | 0 | 0 | Lower pliocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 3 | 25 | 7 | 0 | 1 | 1 | 0 | 57 | 2 | 1 | 3 | 0 |
| 93.50 | 68-502B-22-21,110 | 0 | 0 | 0 | Lower pliocene | FORAM BEARING NANNO MARL | Dominat lithology; numerical abundance | 3 | 25 | 15 | 0 | 1 | 0 | 0 | 50 | 2 | 1 | 3 | 0 |
| 96.40 | 68-502B-22-41,100 | 0 | 0 | 0 | ASH,NANNO, FORAM BEARING MARL | Dominat lithology; numerical abundance | 3 | 15 | 15 | 0 | 1 | 0 | 0 | 58 | 1 | 1 | 5 | 1 |