Worzel, J Lamar; Bryant, William (2005): Smear slide analysis of Hole 10-86 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.230311
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
Smith, L A; McNeely, B; Laury, R; Foreman, H P; Dickinson, K; Capo, R; Beall, A O; Worzel, J Lamar; Bryant, William (1973): Initial Reports of the Deep Sea Drilling Project 10. Initial Reports of the Deep Sea Drilling Project, U.S. Government Printing Office, X, 748 pp, https://doi.org/10.2973/dsdp.proc.10.1973
Further details:
Processed smear slide data base - background and methods. hdl:10013/epic.32353.d001
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 22.874700 * Longitude: -90.962500
Date/Time Start: 1970-02-25T00:00:00 * Date/Time End: 1970-02-25T00:00:00
Minimum DEPTH, sediment/rock: 13.10 m * Maximum DEPTH, sediment/rock: 610.10 m
Event(s):
10-86 * Latitude: 22.874700 * Longitude: -90.962500 * Date/Time: 1970-02-25T00:00:00 * Elevation: -1481.0 m * Penetration: 686.1 m * Recovery: 35.1 m * Location: Gulf of Mexico/BENCH * Campaign: Leg10 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 93.6 m cored; 0 m drilled; 37.5 % 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 | Dolomite | Dol | % | Smear slide analysis | ||
11 | Aragonite | Arg | % | Smear slide analysis | ||
12 | Nannofossils | Nannos | % | Smear slide analysis | ||
13 | Foraminifera | Foram | % | Smear slide analysis | ||
14 | Pteropoda | Pteropoda | % | Smear slide analysis | ||
15 | Chert | Chert | % | Smear slide analysis | fragments | |
16 | Radiolarians | Rad | % | Smear slide analysis | ||
17 | Diatoms | Diatoms | % | Smear slide analysis | ||
18 | Spiculae | Spiculae | % | Smear slide analysis | ||
19 | Quartz | Qz | % | Smear slide analysis | ||
20 | Feldspar | Fsp | % | Smear slide analysis | ||
21 | Zeolite | Zeo | % | Smear slide analysis | ||
22 | Mica | Mica | % | Smear slide analysis | ||
23 | Opaque minerals | Opaque | % | Smear slide analysis | ||
24 | Iron | Fe | % | Smear slide analysis | ||
25 | Volcanic glass | Volc glass | % | Smear slide analysis | ||
26 | Organic matter | OM | % | Smear slide analysis | organic debris |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1123 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 Dol [%] | 11 Arg [%] | 12 Nannos [%] | 13 Foram [%] | 14 Pteropoda [%] | 15 Chert [%] | 16 Rad [%] | 17 Diatoms [%] | 18 Spiculae [%] | 19 Qz [%] | 20 Fsp [%] | 21 Zeo [%] | 22 Mica [%] | 23 Opaque [%] | 24 Fe [%] | 25 Volc glass [%] | 26 OM [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
13.10 | 10-86-1-1,10 | 10 | 35 | 85 | Upper pleistocene | FORAM MUD | Minor lithology; relative abundance | 0 | 0 | 6 | 6 | 23 | 0 | 0 | 0 | 6 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
13.81 | 10-86-1-1,81 | 10 | 35 | 85 | Upper pleistocene | NANNO FORAM MUD | Minor lithology; relative abundance | 0 | 0 | 0 | 23 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
15.66 | 10-86-1-21,116 | 10 | 60 | 85 | Upper pleistocene | NANNO FORAM OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 23 | 23 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
15.70 | 10-86-1-21,120 | 35 | 35 | 60 | Upper pleistocene | NANNO FORAM BEARING ASHY MUD | Minor lithology; relative abundance | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 55 | 0 |
16.40 | 10-86-1-3,40 | 10 | 60 | 60 | Upper pleistocene | SILTY NANNO OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 75 | 6 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
52.65 | 10-86-2-1,65 | 10 | 60 | 60 | Lower pleistocene | SILTY NANNO OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 75 | 6 | 6 | 0 | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
161.10 | 10-86-3-1,10 | 10 | 60 | 60 | Pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 6 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
162.60 | 10-86-3-2,10 | 35 | 60 | 60 | Pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 |
164.10 | 10-86-3-3,10 | 10 | 60 | 60 | Pliocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 |
167.10 | 10-86-3-5,10 | 10 | 60 | 85 | Pliocene | FORAM NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
168.14 | 10-86-3-51,114 | 10 | 60 | 60 | Pliocene | ASHY COCCOLITH OOZE | Minor lithology; relative abundance | 0 | 0 | 0 | 55 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 55 | 0 |
257.60 | 10-86-4-1,60 | 10 | 60 | 85 | Middle pliocene | COCCOLITH OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 2 | 0 | 6 |
258.70 | 10-86-4-2,20 | 10 | 60 | 60 | Middle pliocene | SILTY NANNO OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
260.20 | 10-86-4-3,20 | 35 | 35 | 60 | Middle pliocene | COCCOLITH OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 0 | 2 | 55 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
260.27 | 10-86-4-3,27 | 10 | 60 | 85 | Middle pliocene | SILTY COCCOLITH OOZE | Minor lithology; relative abundance | 2 | 4 | 0 | 42 | 50 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
263.20 | 10-86-4-5,20 | 10 | 60 | 60 | Middle pliocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 6 | 1 | 75 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
263.20 | 10-86-4-5,20 | 10 | 60 | 85 | Middle pliocene | SILTY NANNO OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
372.26 | 10-86-5-11,126 | 10 | 60 | 60 | Lower oligocene | COCCOLITH OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
372.60 | 10-86-5-2,10 | 10 | 60 | 60 | Lower oligocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
373.21 | 10-86-5-2,71 | 35 | 60 | 60 | Lower oligocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 |
373.27 | 10-86-5-2,77 | 60 | 60 | 60 | Lower oligocene | NANNO BEARING ASHY SAND | Minor lithology; relative abundance | 0 | 0 | 0 | 39 | 4 | 0 | 0 | 0 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 53 | 0 |
374.75 | 10-86-5-3,75 | 10 | 60 | 60 | Lower oligocene | NANNO (COCCOLITH) OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
376.27 | 10-86-5-4,77 | 10 | 60 | 85 | Lower oligocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 0 | 0 | 75 | 23 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
441.60 | 10-86-6-CC,0 | 35 | 60 | 60 | FORAM RAD NANNO OOZE | Dominat lithology; relative abundance | 12 | 2 | 0 | 28 | 28 | 0 | 0 | 16 | 0 | 3 | 2 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | |
441.60 | 10-86-6-CC,0 | 35 | 60 | 60 | RAD BEARING FORAM NANNO OOZE | Minor lithology; relative abundance | 16 | 0 | 0 | 33 | 33 | 0 | 0 | 28 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | |
500.20 | 10-86-7-2,70 | 10 | 60 | 60 | Upper paleocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 6 | 0 | 55 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
500.55 | 10-86-7-21,105 | 10 | 60 | 85 | Upper paleocene | NANNO OOZE | Dominat lithology; relative abundance | 0 | 6 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 6 | 0 | 0 | 0 | 0 | 6 | 0 |
501.05 | 10-86-7-3,5 | 10 | 60 | 60 | Upper paleocene | CALCILUTITE (LIME MUD) | Dominat lithology; relative abundance | 0 | 6 | 0 | 6 | 23 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
502.52 | 10-86-7-4,2 | 60 | 60 | 60 | Upper paleocene | FORAM CALCILUTITE | Dominat lithology; relative abundance | 0 | 6 | 0 | 6 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
504.02 | 10-86-7-5,2 | 35 | 60 | 60 | Upper paleocene | NANNO MUD | Dominat lithology; relative abundance | 0 | 6 | 0 | 23 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 6 | 0 |
509.45 | 10-86-8-11,145 | 60 | 60 | 10 | Upper paleocene | ASHY SANDSTONE | Minor lithology; relative abundance | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 75 | 0 |
509.47 | 10-86-8-11,147 | 60 | 60 | 0 | Upper paleocene | VERY FINE TO FINE GRAINED ASHY SAND | Minor lithology; relative abundance | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 2 | 0 | 0 | 6 | 6 | 0 | 8 | 0 | 0 | 75 | 0 |
509.60 | 10-86-8-2,10 | 35 | 60 | 60 | Upper paleocene | NANNO FORAM SILT (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 55 | 55 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 |
509.67 | 10-86-8-2,14 | 10 | 60 | 60 | Upper paleocene | HEMATITIC NANNO MUD (SILTSTONE) | Minor lithology; numerical abundance | 0 | 3 | 0 | 26 | 3 | 0 | 0 | 3 | 0 | 0 | 26 | 0 | 0 | 3 | 0 | 26 | 11 | 0 |
510.00 | 10-86-8-2,50 | 0 | 60 | 60 | Upper paleocene | ASHY NANNO SILTY MUD (CALCILUTITE) | Minor lithology; relative abundance | 0 | 6 | 0 | 55 | 2 | 0 | 0 | 2 | 0 | 2 | 6 | 0 | 1 | 8 | 0 | 0 | 55 | 0 |
510.90 | 10-86-8-21,140 | 35 | 60 | 60 | Upper paleocene | ASH BEARING RAD NANNO SILT | Minor lithology; relative abundance | 0 | 4 | 0 | 32 | 0 | 0 | 0 | 32 | 0 | 13 | 4 | 0 | 0 | 2 | 0 | 0 | 14 | 0 |
511.10 | 10-86-8-3,10 | 35 | 60 | 60 | Upper paleocene | ASH BEARING NANNO RAD MUD | Minor lithology; relative abundance | 0 | 3 | 0 | 31 | 3 | 0 | 0 | 55 | 0 | 13 | 3 | 0 | 0 | 3 | 0 | 0 | 13 | 0 |
513.10 | 10-86-8-4,60 | 35 | 60 | 60 | Upper paleocene | NANNO RAD SILTY MUD | Minor lithology; relative abundance | 0 | 3 | 0 | 27 | 3 | 0 | 0 | 27 | 0 | 27 | 0 | 0 | 0 | 0 | 0 | 0 | 14 | 0 |
513.46 | 10-86-8-4,96 | 60 | 60 | 35 | Upper paleocene | ASHY VERY FINE GRAINED SANDSTONE | Minor lithology; relative abundance | 0 | 6 | 0 | 23 | 0 | 0 | 0 | 6 | 0 | 2 | 2 | 0 | 0 | 6 | 0 | 0 | 57 | 0 |
551.80 | 10-86-9-1,80 | 0 | 60 | 60 | Lower paleocene | NANNO OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 55 | 6 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
552.10 | 10-86-9-11,110 | 0 | 60 | 85 | Lower paleocene | NANNO OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
552.18 | 10-86-9-11,118 | 0 | 60 | 60 | Lower paleocene | NANNO OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 55 | 6 | 0 | 0 | 0 | 0 | 2 | 23 | 0 | 0 | 2 | 0 | 0 | 6 | 0 |
552.65 | 10-86-9-2,15 | 10 | 60 | 60 | Lower paleocene | NANNO SILTY OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 55 | 6 | 0 | 0 | 0 | 0 | 0 | 55 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
553.40 | 10-86-9-2,90 | 0 | 60 | 60 | Lower paleocene | NANNO OOZE (CALCILUTITE) | Dominat lithology; relative abundance | 0 | 6 | 0 | 75 | 6 | 0 | 0 | 0 | 0 | 0 | 23 | 0 | 0 | 6 | 0 | 0 | 0 | 0 |
610.10 | 10-86-10-CC,0 | 0 | 85 | 0 | Lower cretaceous | DOLOMITE | Dominat lithology; relative abundance | 23 | 75 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |